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  • Books  (492)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: G 7148(2. Ex.) ; 10/G 7724 ; M 93.0092/12 ; G 7148(1. Ex.)
    In: Minerals and rocks
    Type of Medium: Monograph available for loan
    Pages: IX, 229 S. : graph. Darst.
    Series Statement: Minerals and rocks 12
    Language: English
    Location: Upper compact magazine
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  • 2
    Monograph available for loan
    Monograph available for loan
    Stroudsburg [u.a.] : Dowden, Hutchinson & Ross
    Associated volumes
    Call number: 10/M 93.0233
    In: Encyclopedia of earth sciences series
    Type of Medium: Monograph available for loan
    Pages: XXI, 1321 S. : Ill., graph. Darst.
    Edition: 5. print.
    ISBN: 0879331801
    Series Statement: Encyclopedia of earth sciences series IVa
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 11/M 93.0094/5
    In: Handbook of strata-bound and stratiform ore deposits ; part II
    Type of Medium: Monograph available for loan
    Pages: XI, 319 S.
    ISBN: 0444414053
    Language: English
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  • 4
    Call number: 9/M 93.0187/1
    In: Developments in economic geology
    In: Association of Exploration Geochemists: Special publication
    Type of Medium: Monograph available for loan
    Pages: XI, 720 S. : graph. Darst.
    ISBN: 0444412808
    Series Statement: Developments in economic geology 1) (Association of Exploration Geochemists special Publication 2
    Language: English
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  • 5
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/M 93.0251A/2
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 6
    Call number: M 93.0154/5 ; 11/G 9206
    In: Developments in petrology
    Type of Medium: Monograph available for loan
    Pages: XI, 272 S.
    ISBN: 0444416587
    Series Statement: Developments in petrology 5
    Language: English
    Location: Upper compact magazine
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  • 7
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/M 93.0251/3
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 8
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/4
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 9
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/2
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 10
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/1 ; 10/G 5218/1 ; 10/M 93.0251A/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: XIV, 442 S.
    Language: English
    Location: Upper compact magazine
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  • 11
    Call number: 12021 ; 10/M 93.0073/1
    In: Developments in geochemistry
    Type of Medium: Monograph available for loan
    Pages: XVIII, 383 S.
    ISBN: 0444416366
    Series Statement: Developments in geochemistry 1
    Language: English
    Location: Upper compact magazine
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  • 12
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 90.1105 ; M 93.0055/5
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: XII, 310 S.
    ISBN: 0444419349
    Series Statement: Developments in precambrian geology 5
    Uniform Title: Fiziko-khimicheskie usloviia obrazovaniia dokembriiskikh zhelezistykh kvartsitov
    Language: English
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  • 13
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 93.0208/7
    In: Developments in economic geology
    Type of Medium: Monograph available for loan
    Pages: XI, 280 S. : Ill., graph. Darst.
    ISBN: 044441567X
    Series Statement: Developments in economic geology 7
    Language: English
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  • 14
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 11/MR 90.0991 ; M 93.0094/4
    In: Handbook of strata-bound and stratiform ore deposits ; part I
    Type of Medium: Monograph available for loan
    Pages: X, 429 S.
    ISBN: 0444414045
    Language: English
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  • 15
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 11/MR 90.0990 ; M 93.0094/3
    In: Handbook of strata-bound and stratiform ore deposits ; part I
    Type of Medium: Monograph available for loan
    Pages: XI, 353 S.
    ISBN: 0444414037
    Language: English
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  • 16
    Monograph available for loan
    Monograph available for loan
    Amsterdam _[u.a.]_ : Elsevier
    Associated volumes
    Call number: 11/M 93.0094/6
    In: Handbook of strata-bound and stratiform ore deposits ; part II
    Type of Medium: Monograph available for loan
    Pages: XVI, 585 S.
    ISBN: 0444414061
    Language: English
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  • 17
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 11/M 93.0094/7
    In: Handbook of strata-bound and stratiform ore deposits ; part II
    Type of Medium: Monograph available for loan
    Pages: xii, 656 S.
    ISBN: 044441407X
    Language: English
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  • 18
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 11/MR 90.0988 ; M 93.0094/1
    In: Handbook of strata-bound and stratiform ore deposits ; part I
    Type of Medium: Monograph available for loan
    Pages: X, 338 S.
    ISBN: 0444414010
    Language: English
    Location: Reading room
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  • 19
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 11/MR 90.0989 ; M 93.0094/2
    In: Handbook of strata-bound and stratiform ore deposits ; part I
    Type of Medium: Monograph available for loan
    Pages: XI, 363 S.
    ISBN: 0444414029
    Language: English
    Location: Reading room
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  • 20
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/G 9222
    In: Reviews in mineralogy
    Description / Table of Contents: Although phyllosilicates are common in almost all types of rocks, their detailed study has not advanced in proportion to their importance. Books and reviews on this subject have been restricted primarily to the areas of clay mineralogy and soils. Such treatments understandably restrict coverage of the occurrences of the macroscopic-size species as well as much of their mineralogical and petrological nature. It was decided at the outset that not all phyllosilicates could be covered in a single book, and the size of this volume addressed only to the micas justifies the original decision. Kaolins, serpentines, chlorites, etc. will have to wait until some later date. This volume attempts to gather together much of our knowledge of micas, the most abundant phyllosilicate, and to indicate promising areas of future research. Chapters 1-3 lay the foundations of the classification, structures, and crystal chemistry of micas. Chapter 4 treats bonding and electrostatic modeling of micas. Chapters 5 and 6 cover spectroscopic and optical properties. Chapters 7-13, the bulk of the volume, are devoted to geochemistry and petrology. These include phase equilibria and the occurrences, chemistry, and petrology of micas in igneous, metamorphic, and sedimentary rocks, pegmatites, and certain ore deposits. Some treatments are exhaustive. All are at the forefront of our present knowledge, and indicate clearly the practical applications'of the study of micas to ascertaining various parameters of origin and crystallization history, as well as the many problems that still exist. The aim of this type of treatment is twofold -- to provide a handy reference volume for teachers and students and to enable researchers to pick more easily those directions and problems for which future research is most needed or is apt to be most productive or most challenging. X-ray powder patterns of micas in the literature are of surprisingly poor quality. The best are collated and supplemented with additional new patterns in the Appendix as an aid to identification.
    Type of Medium: Monograph available for loan
    Pages: xii, 584 S. : Ill., graph. Darst.
    ISBN: 0-939950-17-0 , 978-0-939950-17-1
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 13
    Language: English
    Note: Chapter 1. Classification and Structures of the Micas by S. W. Bailey, p. 1 - 12 Chapter 2. Crystal Chemistry of the True Micas by S. W. Bailey, p. 13 - 60 Chapter 3. The Brittle Micas by Stephen Guggenheim, p. 61 - 104 Chapter 4. Electrostatic Energy Models of Micas by R. F. Giese, Jr., p. 105 - 144 Chapter 5. Spectroscopy of Micas by George R. Rossman. p. 145 - 182 Chapter 6. Optical Properties of Mica Under the Polarizing Microscope by Ray E. Wilcox, p. 183 - 200 Chapter 7. Experimental Phase Relations of the Micas by David A. Hewitt and David R. Wones, p. 201 - 256 Chapter 8. Paragenesis, Crystallochemical Characteristics, and Geochemical Evolution of Micas in Granitic Pegmatites by Petr Cerny and Donald M. Burt, p. 257 - 298 Chapter 9. Micas in Igneous Rocks by J. Alexander Speer, p. 299 - 356 Chapter 10. Micas in Metamorphic Rocks by Charles V. Guidotti, p. 257 - 468 Chapter 11. F-OH and Cl-OH Exchange in Micas with Applications to Hydrothermal Ore Deposits by James L. Munoz, p. 469 - 494 Chapter 12. Illite by Jan Sordori and Dennis D. Eberl, p. 495 - 544 Chapter 13. Glauconite and Celadonite Minerals by I. Edgar Odom, p. 545 - 572 Appendix: X-Ray Power Patterns of Micas p. 573 - 584
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  • 21
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/M 93.0251/5
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 22
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/M 93.0251/4
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 23
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/2 ; 10/G 5218/2/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
    Location: Upper compact magazine
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  • 24
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/3
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 25
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 13/M 97.0131
    In: Elsevier oceanography series
    Type of Medium: Monograph available for loan
    Pages: XIII, 231 S.
    ISBN: 0444414908
    Series Statement: Elsevier oceanography series 14
    Classification:
    Oceanology
    Language: English
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  • 26
    Call number: 9/MR 90.1102 ; MR 90.1103 ; M 93.0055/1
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: VIII, 406 S. : graph. Darst.
    Series Statement: Developments in precambrian geology 1
    Language: English
    Location: Reading room
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  • 27
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 93.0055/2
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: XXIII, 882 S.
    Series Statement: Developments in precambrian geology 2
    Language: English
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  • 28
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
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    Call number: 9/M 93.0055/4
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: XXI 781 S.
    Edition: 2nd impr.
    Series Statement: Developments in precambrian geology 4
    Language: English
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  • 29
    Monograph available for loan
    Monograph available for loan
    Tulsa, Oklah. : American Association of Petroleum Geologists
    Associated volumes
    Call number: 9/M 93.0209
    In: AAPG studies in geology
    Type of Medium: Monograph available for loan
    Pages: VII, 196 S. : graph. Darst.
    ISBN: 0891810099
    Series Statement: AAPG Studies in geology 5
    Language: English
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  • 30
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 93.0003
    In: Developments in economic geology
    Type of Medium: Monograph available for loan
    Pages: XI, 543 S.
    ISBN: 0444418059
    Series Statement: Developments in economic geology 11
    Language: English
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  • 31
    Call number: G 7276 ; 4/M 93.0215
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: XII, 410 S. : graph. Darst.
    ISBN: 9027707944
    Series Statement: NATO ASI series : C, Mathematical and physical sciences 30
    Language: English
    Location: Upper compact magazine
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  • 32
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/M 93.0251A/6
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 33
    Monograph available for loan
    Monograph available for loan
    Madrid : Instituto Tecnológico Geominero de España ; Leiden : Nationaal Natuurhistorisch Museum
    Associated volumes
    Call number: 9/M 97.0173/1
    In: The carboniferous of the world
    Type of Medium: Monograph available for loan
    Pages: 242 S.
    Classification:
    Historical Geology
    Language: English
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  • 34
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: G 8159 ; 10/M 93.0130/1
    In: Handbook of exploration geochemistry
    Type of Medium: Monograph available for loan
    Pages: XIII, 255 S.
    ISBN: 0444419306
    Series Statement: Handbook of exploration geochemistry 1
    Language: English
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  • 35
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 11/M 93.0253/2
    In: Rock-forming minerals
    Type of Medium: Monograph available for loan
    Pages: 668 S.
    Edition: 2nd ed.
    ISBN: 0582465222
    Classification:
    Mineralogy
    Language: English
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  • 36
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Longman
    Associated volumes
    Call number: 11/M 94.0299 ; M 93.0253
    In: Rock-forming minerals
    Type of Medium: Monograph available for loan
    Pages: 919 S.
    Edition: 2nd ed
    ISBN: 0582465265
    Classification:
    Mineralogy
    Language: English
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  • 37
    Call number: 9/M 93.0055/7
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: XII, 475 S.
    Series Statement: Developments in precambrian geology 7
    Language: English
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  • 38
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 93.0055/6
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: XIV, 558 S.
    Series Statement: Developments in precambrian geology 6
    Language: English
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  • 39
    Series available for loan
    Series available for loan
    Warszawa : Panstw. Wyd. Naukowe
    Associated volumes
    Call number: S 91.0236(C-87) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 109 S.
    ISBN: 8388765302
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : C, Geomagnetism 87 = 358
    Language: English
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  • 40
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 04.0008
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: In the two decades since J. Alexander Speer's Zircon chapter in Orthosilicates (Reviews in Mineralogy, Vol. 5), much has been learned about the internal textures, trace-element and isotope geochemistry (both radiogenic and stable) and chemical and mechanical stability of zircon. The application of this knowledge and the use of zircon in geologic studies have become widespread. Today, the study of zircon exists as the pseudo-discipline of "zirconology" that involves materials scientists and geoscientists from across a range of sub-disciplines including stable and radiogenic isotopes, sedimentology, petrology, trace elements and experimental mineralogy. Zirconology has become an important field of research, so much so that coverage of the mineral zircon in a review volume that included zircon as one of many accessory minerals would not meet the needs or interests of the zirconology community in terms of depth or breadth of coverage. The sixteen chapters in this volume cover the most important aspects of zircon-related research over the past twenty-years and highlight possible future research avenues. Finch and Hanchar (Chapter 1) review the structure of zircon and other mineral (and synthetic) phases with the zircon structure. In most rock types where zircon occurs it is a significant host of the rare-earth elements, Th and U. The abundances of these elements and the form of chondrite-normalized rare-earth element patterns may provide significant information on the processes that generate igneous and metamorphic rocks. The minor and trace element compositions of igneous, metamorphic and hydrothermal zircons are reviewed by Hoskin and Schaltegger in Chapter 2. The investigation of melt inclusions in zircon is an exciting line of new research. Trapped melt inclusions can provide direct information of the trace element and isotopic composition of the melt from which the crystal formed as a function of time throughout the growth of the crystal. Thomas et a!. (Chapter 3) review the study of melt inclusions in zircon. Hanchar and Watson (Chapter 4) review experimental and natural studies of zircon saturation and the use of zircon saturation thermometry for natural rocks. Cation diffusion and oxygen diffusion in zircon is discussed by Cherniak and Watson (Chapter 5). Diffusion studies are essential for providing constraints on the quality of trace element and isotope data and for providing estimates of temperature exposure in geological environments. Zircon remains the most widely utilized accessory mineral for U- Th-Pb isotope geochronology. Significant instrumental and analytical developments over the past thirty years mean that zircon has an essential role in early Achaean studies, magma genesis, and astrobiology. Four chapters are devoted to different aspects of zircon geochronology. The first of these four, Chapter 6 by Davis et a!., reviews the historical development of zircon geochronology from the mid-1950s to the present; the following three chapters focus on particular techniques for zircon geochronology, namely ID-TIMS (Parrish and Noble, Chapter 7), SIMS (Ireland and Williams, Chapter 8) and ICP-MS (Kosier and Sylvester, Chapter 9). The application of zircon chronology in constraining sediment provenance.and the calibration ofthe geologic time-scale are reviewed by Fedo et al. (Chapter 10) and Bowring and Schmitz (Chapter 11), respectively. Other isotopic systematics are reviewed for zircon by Kinny and Maas (Chapter 12), who discuss the application of Nd-Sm and Lu-Hf isotopes in zircon to petrogenetic studies, and by Valley (Chapter 13), who discusses the importance of oxygen isotopic studies in traditional and emerging fields of geologic study. As a host of U and Th, zircon is subject to radiation damage. Radiation damage is likely responsible for isotopic disturbance and promotes mechanical instability. There is increasing interest in both the effect of radiation damage on the zircon crystal structure and mechanisms of damage and recrystallization, as well as the structure of the damaged phase. These studies contribute to an overall understanding of how zircon may behave as a waste-form for safe disposal of radioactive waste and are discussed by Ewing et a!. (Chapter 14). The spectroscopy of zircon, both crystalline and metamict is reviewed by Nadsala et a!. (Chapter 15). The final chapter, by Corfu et al. (Chapter 16), is an atlas of internal textures of zircon. The imaging of internal textures in zircon is essential for directing the acquisition of geochemical data and to the integrity of conclusions reached once data has been collected and interpreted. This chapter, for the first time, brings into one place textural images that represent common and not so common textures reported in the literature, along with brief interpretations of their significance. There is presently no comparable atlas. It is intended that this chapter will become a reference point for future workers to compare and contrast their own images against. The chapters in this volume of Reviews in Mineralogy and Geochemistry were prepared for presentation at a Short Course, sponsored by the Mineralogical Society of America (MSA) in Freiburg, Germany, April 3-4, 2003. This preceded a joint meeting of the European Union of Geology, the American Geophysical Union and the European Geophysical Society held in Nice, France, April 6-11, 2003.
    Type of Medium: Monograph available for loan
    Pages: XVII, 500 S.
    ISBN: 0-939950-65-0 , 978-0-939950-65-2
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 53
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Structure and chemistry of zircon and zircon-group minerals by Robert J. Finch and John M. Hanchar, p. 1 - 26 Chapter 2. The composition of zircon and igneous and metamorphic petrogenesis by Paul W. O. Hoskin and Urs Schaltegger, p. 27 - 62 Chapter 3. Melt inclusions in zircon by J. B. Thomas, Robert J. Bodnar, Nobumichi Shimizu, and Craig A. Chesner, p. 63 - 88 Chapter 4. Zircon saturation thermometry by John M. Hanchar and E. Bruce Watson, p. 89 - 112 Chapter 5. Diffusion in zircon by Daniele J. Cherniak and E. Bruce Watson, p. 113 - 144 Chapter 6. Historical development of zircon geochronology by Donald W. Davis, Ian S. Williams, and Thomas E. Krogh, p. 145 - 182 Chapter 7. Zircon U-Th-Pb geochronology by isotope dilution—thermal ionization mass spectrometry (ID-TIMS) by Randall R. Parrish and Stephen R. Noble, p. 183 - 214 Chapter 8. Considerations in zircon geochronology by SIMS by Trevor R. Ireland and Ian S. Williams, p. 215 - 242 Chapter 9. Present trends and the future of zircon in geochronology: laser ablation ICPMS by Jan Kosler and Paul J. Sylvester, p. 243 - 276 Chapter 10. Detrital zircon analysis of the sedimentary record by Christopher M. Fedo, Keith N. Sircombe, and Robert H. Rainbird, p. 277 - 304 Chapter 11. High-precision U-Pb zircon geochronology and the stratigraphic record by Samuel A. Bowring and Mark D. Schmitz, p. 305 - 326 Chapter 12. Lu-Hf and Sm-Nd isotope systems in zircon by Peter D. Kinny and Roland Maas, p. 327 - 342 Chapter 13. Oxygen isotopes in zircon by John W. Valley, p. 343 - 386 Chapter 14. Radiation effects in zircon by Rodney C. Ewing, Alkiviathes Meldrum, LuMin Wang, William J. Weber, and L. René Corrales, p. 387 - 426 Chapter 15. Spectroscopic methods applied to zircon by Lutz Nasdala, Ming Zhang, Ulf Kempe, Gérard Panczer, Michael Gaft, Michael Andrut, and Michael Plotze, p. 427 - 468 Chapter 16. Atlas of zircon textures by Fernando Corfu, John M. Hanchar, Paul W.O. Hoskin, and Peter Kinny, p. 469 - 500
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    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 11/M 93.1115 ; M 93.0250/2
    In: Mineral deposits of Europe
    Type of Medium: Monograph available for loan
    Pages: xi, 304 S.
    ISBN: 0900488638
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 11/M 93.1114 ; M 93.0250/1
    In: Mineral deposits of Europe
    Type of Medium: Monograph available for loan
    Pages: xi, 362 S.
    ISBN: 0900488441
    Classification:
    Deposits
    Language: English
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  • 43
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    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 11/M 04.0178
    In: Rock-forming minerals
    Type of Medium: Monograph available for loan
    Pages: XX, 758 S.
    Edition: 2nd ed.
    ISBN: 1862391424
    Classification:
    Mineralogy
    Language: English
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  • 44
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: M 94.0161 / Regal 11
    In: Reviews in mineralogy
    Description / Table of Contents: Fourteen years ago the American Geological Institute (AGI) sponsored a Short Course on Chain Silicates. At that time, a substantial amount was known about the crystal chemistry and phase equilibria of pyroxenes, and this knowledge has been of fundamental importance in guiding research on pyroxenes in the years following the AGI Short Course. In 1966, single-crystal x-ray diffractometry was well advanced and good crystal structure refinements were available for jadeite, spodumene, hypersthene, c1inoferrosi1ite, orthoferrosi1ite, and omphacite; the distinction between the c1inoenstatite (pigeonite) and diopside (augite) structures had been established, and the structure of protoenstatite was known, although some doubt existed about the space group of protoenstatite. Phase diagrams for several joins in the pyroxene quadrilateral had been published, but often equilibrium had not been established in the experiments and not enough was known about the effects of pressure, oxygen fugacity, and non-quad elements such as aluminum on the phase equilibria. Also, inversion relations of Ca-poor pyroxenes were not well understood, and petrologists had just become aware of the effect of stress on orthoto-clinopyroxene transitions. In 1966 few of us would have guessed how-much new data and new analytical results would become available in the next fourteen years. Although most, if not all, of the important instrumental techniques we use today were available in 1966, the truly spectacular development and application of these techniques did not take place until the Apollo 11 samples and the attendant funding from NASA became available. Pyroxene research has profited immensely from the application of Mossbauer, optical, and infrared spectroscopy, x-ray and electron diffraction, transmission electron microscopy, automated electron microprobes, and digital computers. During these years experimentalists extended the capabilities of their equipment to examine the behavior of pyroxenes under conditions of controlled oxygen fugacity, pressure, and temperature, conditions more nearly like those under which pyroxenes crystallize in natural systems. Looking back, one remembers the excitement of seeing the first lunar samples. We were surprised at the large amounts of pigeonite and the quality of crystals unaffected by water or the presence of sodium. The influence of the lunar program on pyroxene research was extraordinary, and our understanding of pyroxene relationships in terrestrial occurrences benefited tremendously because the lunar pyroxenes provided a basis for comparison with the more complex chemical and structural behavior of terrestrial environments. Probably the most impressive development in the early lunar sample studies was the application of transmission electron microscopy to mineralogy. We were able to see exsolution and other textural features in crystals that looked homogeneous in the optical microscope, thus opening up a wide range of research possibilities that had not existed previously. Advanced crystal growth experiments, detailed phase equilibria, x-ray diffraction at high temperatures, and statistical analyses of microprobe data were all applied to lunar pyroxenes and then extended to terrestrial and meteorite investigations, making this period one of the most productive in history. In the compilation of this volume, an attempt has been made to review the essential aspects of pyroxene research, primarily those of the last ten or fifteen years. Although the largest fraction of pyroxene research has been performed in the U.S.A., significant advances have been made in other countries, particularly in Europe, Japan, Canada, and Australia, with interest and activity in these countries probably growing at a faster rate than in the United States. Recently, Deer, Howie and Zussman (DHZ) published a second edition of their volume in the Rock-Forming Minerals series, Single-Chain Silicates, Vol. 2A (John Wiley, New York, 1978). The present volume is intended to be complementary to DHZ and to provide material covered lightly or not at all in DHZ, such as electron microscopy, spectroscopy, and detailed thermodynamic treatments. However, because the range of pyroxene research has grown so much in recent years, there still are important areas not covered comprehensively in either of these volumes. Some of these areas are kinetics, diffusion, crystal defects, deformation, and nonsilicate pyroxene crystal chemistry. Because of these omissions and because this volume is intended for use with the MSA Short Course on Pyroxenes to be held at Emory University in conjunction with the November, 1980 meeting of the Society, a Symposium on Pyroxenes was organized by J. Stephen Huebner for the meeting that is designed to present the latest research results on several different topics, including those above. With DHZ, this volume, and publications from the Symposium, the student of pyroxenes should be well-equipped to advance our knowledge of pyroxenes in the decades ahead.
    Type of Medium: Monograph available for loan
    Pages: x, 525 S.
    Edition: 2nd print.
    ISBN: 0-939950-07-3 , 978-0-939950-07-2
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 7
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Introduction by Charles T. Prewitt, p. 1 - 4 Chapter 2. Crystal Chemistry of Silicate Pyroxenes by Maryellen Cameron and James J. Papike, p. 5 - 92 Chapter 3. Pyroxene Spectroscopy by George R. Rossman, p. 93 - 116 Chapter 4. Subsolidus Phenomena in Pyroxene by Peter R. Buseck, Gordon L. Nord, Jr., and David R. Veblen, p. 117 - 212 Chapter 5. Pyroxene Phase Equilibria at Low Pressure by J. Stephen Huebner, p. 213 - 288 Chapter 6. Phase Equilibria of Pyroxenes at Pressure 〉1 Atmosphere by Donald H. Lindsley, p. 289 - 308 Chapter 7. Phase Equilibria at High Pressure of Pyroxenes Containing Monovalent and Trivalent Ions by Tibor Gasparik and Donald H. Lindsley, p. 309 - 340 Chapter 8. Thermodynamics of Pyroxenes by J. E. Grover, p. 341 - 418 Chapter 9. The Composition Space of Terrestrial Pyroxenes - Internal and External Limits by Peter Robinson, p. 419 - 494 Chapter 10. Pyroxene Mineralogy of the Moon and Meteorites by James J. Papike, p. 495 - 525
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    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 94.0162
    In: Reviews in mineralogy
    Description / Table of Contents: Geochemistry is a science that is based on an understanding of chemical processes in the earth. One of the principal tools available to the chemist for understanding systems at equilibrium is thermodynamics. The awareness and application of thermodynamic techniques has increased at a very fast pace in geosciences; in fact, one may be so bold as to say that thermodynamics in geology has reached the "mature" stage, although much future thermodynamic research is certainly needed. However, the natural processes in the earth are often sluggish enough that a particular system may not reach equilibrium. This observation is being supported constantly by new experimental and field data available to the geochemist e.g. the non-applicability of the phase rule in some assemblages, the compositional inhomogeneities of mineral grains, the partial reaction rims surrounding original minerals, the lack of isotopic equilibration or the absence of minerals (e.g. dolomite), which should be present according to thermodynamics. The need to apply kinetics has produced a large number of papers dealing with kinetics in geochemistry. As an initial response to this growing field, a conference on geochemical transport and kinetics was conducted at Airlie House, VA, in 1973, sponsored by the Carnegie Institution of Washington. The papers there dealt with several kinetic topics including diffusion, exsolution, metasomatism and metamorphic layering. Since 1973 the number of kinetic papers has continued to increase greatly. Therefore, the time is ripe for a Short Course in Kinetics, which brings together the fundamentals needed to explain field observations using kinetic data. It is hoped that this book may serve, not only as a reference for researchers dealing with the rates of geochemical processes, but also as a text in courses on geochemical kinetics. One of us has found this need of a text in teaching a graduate course on geochemical kinetics at Harvard and at Penn State during the past several years. Finally, it is our hope that the book may itself further even more research into the rates of geochemical processes and into the quantification of geochemical observations. The book is organized with a rough temperature gradient in mind, i.e. low temperature kinetics at the beginning and igneous kinetics at the end (no prejudices are intended with this scheme!). However, the topics in each chapter are general enough that they can be applied often to any geochemical domain: sedimentary, metamorphic or igneous. The theory of kinetics operates at two complementary levels: the phenomenological and the atomistic. The former relies on macroscopic variables (e.g. temperature or concentrations) to describe the rates of reactions or the rates of transport; the latter relates the rates to the basic forces operating between the particular atomic or molecular species of any system. This book deals with both descriptions of the kinetics of geochemical processes. Chapter one sets the framework for the phenomenological theory of reaction rates. If any geochemical reaction is to be described quantitatively, the rate law must be experimentally obtained in a kinetically sound manner and the reaction mechanism must be understood. This applies to heterogeneous fluid-rock reactions such as those occurring during metamorphism, hydrothermal alteration or weathering as well as to homogeneous reactions. Chapter 2 extends the theory to the global kinetics of geochemical cycles. This enables the kinetic concepts of stability and feedback to be applied to the cycling of elements in the many reservoirs of the earth. Chapter 3 applies the phenomenological treatment of chapter 1 to diagenesis and weathering. The rate of dissolution of minerals as well as the chemical evolution of pore waters are discussed. The atomistic basis of rates of reaction, transition state theory, is introduced in Chapter 4. Transition state theory can be applied to relate the rate constants of geochemical reactions to the atomic processes taking place. This includes not only homogeneous reactions but also reactions that occur at the surface of minerals. Chapter 5 discusses the theory of irreversible thermodynamics and its application to petrology. The use of the second law of thermodynamics along with the expressions for the rate of entropy production in a system have been used successfully since 1935 to describe kinetic phenomena. The chapter applies the concepts to the growth of minerals during metamorphism as well as to the formation of differentiated layers (banding) in petrology. Chapter 6 describes the phenomenological theory of diffusion both in aqueous solutions and in minerals. In particular, the multicomponent nature of diffusion and its consequence in natural systems is elaborated. Chapter 7 provides the atomistic basis for the rates of reactions in minerals. Understanding of the rates of diffusion, conduction, order-disorder reactions or exsolution in minerals depends on proper description of the defects in the various mineral structures. Chapter 8 provides the kinetic theory of crystal nucleation and growth. While many of the concepts in the chapter can be applied to aqueous systems, the emphasis is on igneous processes occurring during crystallization of a melt. To fully understand both the mineral composition as well as the texture of igneous rocks, the processes whereby new crystals form and grow must be quantified by using kinetic theory. Due to space and time limitations (kinetics!) some topics have not been covered in detail. In particular, the mathematical solution of diffusion or conduction equations is discussed very well by Crank in his book, Mathematics of Diffusion, and so is not covered to a great extent here. The treatment of fluid flow (e.g. convection) is also not covered in the text.
    Type of Medium: Monograph available for loan
    Pages: x, 398 S.
    ISBN: 0-939950-08-1 , 978-0-939950-08-9
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 8
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Rate Laws of Chemical Reactions by Antonio C. Lasaga, p. 1 - 68 Chapter 2. Dynamic Treatment of Geochemical Cycles: Global Kinetics by Antonio C. Lasaga, p. 69 - 110 Chapter 3. Kinetics of Weathering and Diagenesis by Robert A. Berner, p. 111 - 134 Chapter 4. Transition State Theory by Antonio C. Lasaga, p. 135 - 170 Chapter 5. Irreversible Thermodynamics in Petrology by George W. Fisher and Antonio C. Lasaga, p. 171 - 210 Chapter 6. Diffusion in Electrolyte Mixtures by David E. Anderson, p. 211 - 260 Chapter 7. The Atomistic Basis of Kinetics: Defects in Minerals by Antonio C. Lasaga, p. 261 - 320 Chapter 8. Kinetics of Crystallization of Igneous Rocks by R. James Kirkpatrick, p. 321 - 398
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    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(B-34) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 207 S.
    ISBN: 8388765396
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 34 = 367 : monograph volume
    Classification:
    Seismology
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Melbourne [u.a.] : Lonely Planet Publ.
    Call number: 1.8/N 01.0537
    Type of Medium: Monograph available for loan
    Pages: 972 S.
    Edition: 3rd ed.
    ISBN: 1864501928
    Series Statement: Lonely planet travel guidebooks
    Classification:
    E.5.
    Language: English
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    Call number: 1.2/Q 3451
    Type of Medium: Monograph available for loan
    Pages: 778 S.
    ISBN: 204011954X
    Language: Spanish
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    Monograph available for loan
    Monograph available for loan
    New York, NY : Freeman
    Call number: 12/M 02.0062 ; AWI A3-02-0023 ; PIK N 456-02-0005
    Type of Medium: Monograph available for loan
    Pages: xxi, 465 S. , zahlr. Ill., graph. Darst., Kt. , 28 cm
    ISBN: 0716737418
    Classification:
    D 4..
    Language: English
    Note: Contents: Preface. - PART 1 FRAMEWORK OF CLIMATE SCIENCE. - 1 Overview of Climate Science. - Climate and Climate Change. - 1-1 Geologic Time. - 1-2 How This Book Is Organized. - Development of Climate Science. - 1-3 How Scientists Study Climate Change. - Overview of the Climate System. - 1-4 Components of the Climate System. - 1-5 Climate Forcing. - 1-6 Climate System Responses. - 1-7 Time Scales of Forcing versus Response. - 1-8 Response Rates and Interactions Within the Climate System. - 1-9 Feedbacks in the Climate System. - Tools Of Climate Science: Temperature Scales. - 2 Earth's Climate System Today. - Heating Earth. - 2-1 Incoming Solar Radiation. - 2-2 Receipt and Storage of Solar Heat. - 2-3 Heat Transformation. - Heat Transfer in Earth's Atmosphere. - 2-4 Overcoming Stable Layering in the Atmosphere. - 2-5 Tropical-Subtropical Atmospheric Circulation. - 2-6 Atmospheric Circulation at Middle and High Latitudes. - Heat Transfer in Earth's Oceans. - 2-7 The Surface Ocean. - 2-8 Deep-Ocean Circulation. - Ice on Earth. - 2-9 Sea Ice. - 2-10 Glacial Ice. - Earth's Biosphere. - 2-11 Response of the Biosphere to the Physical Climate System. - 2-12 Effects of the Biosphere on the Climate System. - Looking Deeper into Climate Science: The Structure of Earth's Atmosphere. - Climate Interactions and Feedbacks: Albedo/Temperature. - Climate Interactions and Feedbacks: Water in the Climate System. - Climate Interactions and Feedbacks: Water Vapor. - Looking Deeper into Climate Science: The Conolis Effect. - Climate Interactions and Feedbacks: Vegetation-Climate Feedbacks. - 3 Climate Archives, Oata, and Models. - Climate Archives. - 3-1 Types of Archives. - 3-2 Dating Climate Records. - 3-3 Climate Resolution. - Climate Data. - 3-4 Biotic Data. - 3-5 Geological and Geochemical Data. - Climate Models. - 3-6 Physical Climate Models. - 3-7 Geochemical (Mass Balance) Models. - PART II TECTONIC-SCALE CLIMATE CHANGE. - 4 CO2 and Long-term Climate. - Greenhouse Worlds. - The Faint Young Sun Paradox. - Carbon Exchanges between Rocks and the Atmosphere. - 4-1 Volcanic Input of Carbon from Rocks to the Atmosphere. - 4-2 Chemical Weathering Removal of CO2 from the Atmosphere. - Climate Factors That Control Chemical Weathering. - Chemical Weathering: Earth's Thermostat?. - Is Life the Ultimate Control on Earth's Thermostat?. - 4-3 The Gaia Hypothesis. - Climate Debate: A Snowball Earth?. - Looking Deeper into Climate Science: The Organic Carbon Subcycle. - 5 Plate Tectonics and Climate. - Plate Tectonics. - 5-1 Structure and Composition of Tectonic Plates. - 5-2 Evidence of Past Plate Motions. - The Polar Position Hypothesis. - 5-3 Glaciations and Continental Positions since 500 Myr Ago. - Modeling Climate on the Supercontinent Pangaea. - 5-4 Input to the Model Simulation of Pangaean Climate. - 5-5 Output from the Model Simulation of Pangaean Climate. - Tectonic Control of CO2 Input: The BLAG Spreading Rate Hypothesis. - 5-6 Control of CO2 Input by Seafloor Spreading. - 5-7 Initial Evaluation of the BLAG Spreading Rate Hypothesis. - Tectonic Control of CO2 Removal: The Uplift Weathering Hypothesis. - 5-8 Rock Exposure and Chemical Weathering. - 5-3 Uplift and Chemical Weathering. - What Controls Chemical Weathering?. - 5-10 Weathering: Climate Forcing and Feedback. - Looking Deeper into Climate Science: Brief Glatiation 430 Myr Ago. - 6 Greenhouse Earth. - What Explains Greenhouse Warmth 100 Myr Ago?. - 6-1 Model Simulations of a Greenhouse World. - 6-2 What Explains the Data-Model Mismatch?. - Sea Level Changes and Climate. - 6-3 Causes of Tectonic-Scale Changes in Sea Level. - 6-4 Effect of Sea Level Changes on Climate. - Asteroid Impacts. - Climate Interactions and Feedbacks: The Effect of CO2 on Climate. - Looking Deeper into Climate Science: Calculating Changes in Sea Level. - 7 Back into the Icehouse: The Last 55 Million years. - Global Climate Change Since 55 Myr Ago. - 7-1 Evidence from Ice and Vegetation. - 7-2 Oxygen Isotope Data. - Why Did Global Climate Cool over the Last 55 Myr?. - 7-3 Evaluating the BLAG Spreading Rate Hypothesis. - 7-4 Evaluating the Uplift Weathering Hypothesis. - 7-5 Evaluating the Ocean Heat Transport Hypothesis. - 7-6 Causes of Brief Tectonic-Scale Climate Change. - Understanding and Predicting Tectonic Climate Change. - Tools Of Climate Science: Oxtygen Isotope Ratios (δ18O). - Climate Debate: The Timing of Uplift in Western North America. - Looking Deeper into Climate Science: Is 87Sr/86Sr an Index of Chemical Weathering?. - PART III ORBITAL-SCALE CLIMATE CHANGE. - 8 Astronomical Control of Solar Radiation. - Earth's Orbit Today. - 8-1 Earth's Tilted Axis of Rotation and the Seasons. - 8-2 Earth's Eccentric Orbit: Changes in the Distance Between Earth and Sun. - Long-Term Changes in Earth's Orbit. - 8-3 Changes in Earth's Axial Tilt Through Time. - 8-4 Changes in Earth's Eccentric Orbit Through Time. - 8-5 Precession of Solstices and Equinoxes around Earth's Orbit. - Changes in Insolation Received on Earth. - 8-6 Insolation Changes by Month and Season. - 8-7 Insolation Changes According to Caloric Season. - Looking for Orbital-Scale Changes in Climate Records. - 8-8 Time Series Analysis. - 8-9 Aliasing of Climate Records. - 8-10 Tectonic-Scale Changes in Earth's Orbit. - Tools Of Climate Science: Cycles and Modulation. - Looking Deeper into Climate Science: Earth's Precession as a Sine Wave. - 9 Insolation Control of Monsoons. - Monsoon Circulations. - 9-1 Orbital-Scale Control of Summer Monsoons. - Evidence of Orbital-Scale Changes in Summer Monsoons. - 3-2 "Stinky Muds" in the Mediterranean. - 9-3 Freshwater Diatoms in the Tropical Atlantic. - 9-4 Upwelling in the Equatorial Atlantic. - Refinements of the Orbital Monsoon Hypothesis. - 9-5 Lag of Monsoons Behind Summer Insolation. - 9-6 Clipped Monsoon Responses and Monsoon Harmonics. - Monsoon Forcing Earlier in Earth's History. - 8-7 Monsoons on Pangaea 200 Myr Ago. - 9-8 Joint Tectonic and Orbital Control of Monsoons. - 10 Insolation Control of Ice Sheets. - What Controls the Size of Ice Sheets?. - 10-1 Orbital-Scale Control of Ice Sheets. - The Milankovitch Theory. - Modeling the Behavior of Ice Sheets. - 10-2 Insolation Control of Ice Sheet Size. - 10-3 Ice Sheet Lags behind Summer Insolation Forcing. - 10-4 Delayed Bedrock Response Beneath Ice Sheets. - 10-5 Full Cycle of Ice Growth and Decay. - 10-6 Ice Slipping and Calving. - Northern Hemisphere Ice Sheet History. - 10-7 Conceptual Model: Evolution of Ice Sheet Cycles. - 10-8 Evidence from δ18O: How Ice Sheets Actually Evolved. - 10-9 Confirming Ice Volume Changes: Coral Reefs and Sea Level. - 10-10 Using Astronomical and δ18O Signals as a Chronometer. - Looking Deeper into Climate Science: Ice Volume Response to Insolation. - Climate Debate: Antarctic Deglaciation 3 Myr Ago?. - Looking Deeper into Climate Science: Sea Level on Uplifting Islands. - 11 Orbital-Scale Changes in Carbon Dioxide and Methane. - Ice Cores. - 11-1 Drilling and Dating Ice Cores. - 11-2 Trapping Gases in the Ice. - Orbital-Scale Changes in Methane. - Orbital-Scale Changes in CO2. - 11-3 Physical Oceanographic Explanations of CO2 Changes. - 11-4 Orbital-Scale Carbon Reservoirs. - 11-5 Tracking Carbon through the Climate System. - 11-6 Can δ13C Evidence Detect Glacial Changes in Carbon Reservoirs?. - 11-7 Pumping of Carbon into the Deep Ocean during Glaciations. - 11-8 Changes in the Circulation of Deep Water during Glaciations. - Tools Of Climate Science: Carbon Isotope Ratios (δ13C). - Climate Debate: Do Winds Fertilize the Glacial Ocean?. - 12 Orbital-Scale Interactions in the Climate System. - Orbital-Scale Forcing and Response Revisited. - Ice-Driven Climate Responses. - 12-1 Ice-Driven Responses in High Northern Latitudes. - 12-2 Orbital Cycles in Regions Remote fro
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    Call number: 21/STR 02/01
    In: Scientific technical report
    Type of Medium: GFZ publications
    Pages: 36 S.
    Series Statement: Scientific technical report / Geoforschungszentrum Potsdam 02/01
    Classification:
    A. 1.7.
    Language: English
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    Call number: 12/N 02.0113 ; PIK N 075-03-0318
    Type of Medium: Monograph available for loan
    Pages: xxvi, 651 S.
    ISBN: 3540422390
    Classification:
    D. 4.
    Language: English
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    Stuttgart : Wiss. Verl.-Ges.
    Call number: MOP 45472 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 632 S.
    ISBN: 380470509X
    Series Statement: Books of the journal Naturwissenschaftliche Rundschau
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    Call number: 8/M 02.0587 ; M 09.0416 ; M 13.0207
    Type of Medium: Monograph available for loan
    Pages: XVII, 834 S.
    ISBN: 3540679626
    Classification:
    B.6.
    Language: English
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  • 54
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    New York, NY [u.a.] : Reinhold
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    Call number: 12/6412 ; PIK N 456-99-0143
    In: Encyclopedia of earth sciences series
    Type of Medium: Monograph available for loan
    Pages: XV, 1200 S. : Ill., graph. Darst.
    Series Statement: Encyclopedia of earth sciences series 2
    Language: English
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  • 55
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    Amsterdam [u.a.] : Elsevier
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    Call number: 11/G 9166
    In: Developments in petrology
    Type of Medium: Monograph available for loan
    Pages: X, 239 S. : Ill., graph. Darst.
    Series Statement: Developments in petrology 10
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  • 56
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    New York [u.a.] : Plenum Pr.
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    Call number: 4/M 02.0207
    In: Topics in geobiology
    Type of Medium: Monograph available for loan
    Pages: xviii, 458 S.
    ISBN: 0306464675
    Series Statement: Topics in geobiology 17
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  • 57
    Call number: NBM 02.0251
    In: Professional paper
    Type of Medium: Non-book medium
    Pages: 2 CD-ROM's
    Edition: Version 1.0
    Series Statement: Professional paper / U. S. Geological Survey 1625-B
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  • 58
    Call number: 9/M 02.0292
    In: Geological Society special publication
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    Pages: 408 S.
    ISBN: 1862390800
    Series Statement: Geological Society special publication 184
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  • 59
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    London [u.a.] : Routledge
    Call number: 12/M 02.0263 ; AWI G5-02-0134
    Type of Medium: Monograph available for loan
    Pages: xviii, 267 S.
    Edition: 1st publ.
    ISBN: 0415198410
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  • 60
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    London [u.a.] : Springer
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    Call number: 5/M 02.0264 ; AWI G5-02-0133
    In: Springer Praxis books in geophysical sciences
    Type of Medium: Monograph available for loan
    Pages: xx, 290 S.
    ISBN: 3540426469
    Series Statement: Springer Praxis books in geophysical sciences
    Uniform Title: Le quaternaire g´eologie et milieux naturels
    Classification:
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    San Francisco : Freeman
    Call number: 4/M 02.0329
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    Pages: xxiii, 121 S. + 1 CD-ROM, Erg. [CD-ROM defekt und Erg. fehlt - 05.05.2008!]
    Edition: 3rd ed., 2nd print.
    ISBN: 0716735040
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  • 62
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    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(88) / Regal 35
    In: Materialy i prace
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    Pages: 93 S.
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  • 63
    Call number: SR 91.0236(B-26) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 83 S.
    ISBN: 8388765108
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  • 64
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    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(87) / Regal 35
    In: Materialy i prace
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    Call number: SR 91.0236(83) / Regal 35
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    Call number: SR 91.0236(96) / Regal 35
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  • 67
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    Warszawa : Panstw. Wyd. Naukowe
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    Call number: S 91.0236(B-29) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 98 S.
    ISBN: 8388765221
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  • 68
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    Warszawa : Panstw. Wyd. Naukowe
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    In: Materialy i prace
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    Call number: SR 91.0236(85) / Regal 35
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    Pages: 79 S.
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    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(A-12) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 64 S.
    ISBN: 830103839X
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    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(A-7) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 63 S.
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    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(A-3) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 71 S.
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    Call number: 8/M 02.0392
    In: NATO science series
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    Pages: xvi, 207 S.
    ISBN: 1402006535
    Series Statement: NATO sciences series : IV, Earth and environmental sciences 9
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    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(A-2) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 190 S.
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : A, Physics of the earth's interior 2 = 101
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    Call number: SR 91.0236(A-15) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 80 S.
    ISBN: 8301059931
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : A, Physics of the earth's interior 15 = 174
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    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-6,2) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 97 S.
    ISBN: 8301034785
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 6 = 152
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    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-6,1) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 45 S.
    ISBN: 8301030100
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    Call number: SR 91.0236(B-6,4) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 172 S.
    ISBN: 8301038829
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    Call number: SR 91.0236(G-1) / Rgal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 54 S.
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : G, Numerical methods in geophysics 1 = 110
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    Call number: SR 91.0236(G-2) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 59 S.
    ISBN: 8301035870
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : G, Numerical methods in geophysics 2 = 143
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    Call number: SR 91.0236(B-7,1) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 50 S.
    ISBN: 8301040157
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 7 = 161
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  • 82
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    Berlin [u.a.] : Springer
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    Call number: 10/M 92.1196 ; 12169 ; 12265
    In: Minerals and rocks
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    Pages: XII, 252 S. : Ill.
    ISBN: 3540102086
    Series Statement: Minerals and rocks 15
    Classification:
    Petrology, Petrography
    Language: English
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    Princeton : Princeton Univ. Pr.
    Call number: 10/M 92.1066 ; M 93.0029 ; PIK N 454-94-0391
    Type of Medium: Monograph available for loan
    Pages: xii, 582 S.
    ISBN: 0691083487
    Series Statement: Princeton series in geochemistry
    Classification:
    Geochemistry
    Language: English
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  • 84
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    Oxford : Blackwell Scientific Publications
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    Call number: 9/G 9202
    In: Special publications / the Geological Society, London, Volume 13
    Description / Table of Contents: Preface The proposal that ophiolites are on-land fragments of oceanic lithosphere has been with us for over 20 years and has been widely accepted by the Earth Sciences' community. Despite this, many oceanographers are reluctant to use ophiolite data. Their argument (and it comes largely from the geological rather than geophysical oceanographers) is that 'Even if ophiolites are on-land fragments of oceanic lithosphere, they must be atypical for otherwise they would have been subducted and not obducted'. So they conclude that, although the study of ophiolites is perfectly acceptable in its own right, its results should not be used in the investigation of present-day, in-situ oceanic lithosphere--i.e, the invoking of 'reversed uniformitarianism' is not acceptable. However using uniformitarian principles to interpret ophiolites from present-day oceanic lithosphere studies is equally problematical for (i) petrological/geochemical studies of ocean-floor rocks are based on widely spaced boreholes of limited depth and dredge-haul sampling, (ii) geophysical data can only detect large-scale phenomena and are open to various interpretations, and (iii) direct observations from submersibles are still very limited. Such circumstances should have drawn the two groups of workers closer together.
    Type of Medium: Monograph available for loan
    Pages: VI, 413 Seiten , Illustrationen
    ISBN: 0632012196
    Series Statement: Special publications / the Geological Society, Londonn 13
    Language: English
    Note: I. Nature and Formation of Oceanic Lithosphere --- Magma Chambers: Products and Processes --- J. A. Orcutt, M. Burnett, and J. S. McClain: Evolution of the ocean crust: results from recent seismic experiments / Geological Society, London, Special Publications, 13:7-16, doi:10.1144/GSL.SP.1984.013.01.01 --- M. R. Fisk: Depths and temperatures of mid-ocean-ridge magma chambers and the composition of their source magmas / Geological Society, London, Special Publications, 13:17-23, doi:10.1144/GSL.SP.1984.013.01.02 --- M. F. J. Flower: Spreading-rate parameters in ocean crust: analogue for ophiolite? / Geological Society, London, Special Publications, 13:25-40, doi:10.1144/GSL.SP.1984.013.01.03 --- J. D. Smewing, N. I. Christensen, I. D. Bartholomew, and P. Browning: The structure of the oceanic upper mantle and lower crust as deduced from the northern section of the Oman ophiolite / Geological Society, London, Special Publications, 13:41-53, doi:10.1144/GSL.SP.1984.013.01.04 --- R. T. Gregory: Melt percolation beneath a spreading ridge: evidence from the Semail peridotite, Oman / Geological Society, London, Special Publications, 13:55-62, doi:10.1144/GSL.SP.1984.013.01.05 --- J. S. Pallister: Parent magmas of the Semail ophiolite, Oman / Geological Society, London, Special Publications, 13:63-70, doi:10.1144/GSL.SP.1984.013.01.06 --- P. Browning: Cryptic variation within the Cumulate Sequence of the Oman ophiolite: magma chamber depth and petrological implications / Geological Society, London, Special Publications, 13:71-82, doi:10.1144/GSL.SP.1984.013.01.07 --- D. Elthon, J. F. Casey, and S. Komor: Cryptic mineral-chemistry variations in a detailed traverse through the cumulate ultramafic rocks of the North Arm Mountain massif of the Bay of Islands ophiolite, Newfoundland / Geological Society, London, Special Publications, 13:83-97, doi:10.1144/GSL.SP.1984.013.01.08 --- Fracture Zones --- R. S. White: Atlantic oceanic crust: seismic structure of a slow-spreading ridge / Geological Society, London, Special Publications, 13:101-111, doi:10.1144/GSL.SP.1984.013.01.09 --- J. M. Auzende, G. Ceuleneer, G. Cornen, T. Juteau, Y. Lagabrielle, G. Lensch, C. Mevel, A. Nicolas, H. Prichard, A. Ribeiro, E. Ruellan, and J. R. Vanney: Intraoceanic tectonism on the Gorringe Bank: observations by submersible / Geological Society, London, Special Publications, 13:113-120, doi:10.1144/GSL.SP.1984.013.01.10 --- J. Honnorez, C. Mevel, and R. Montigny: Occurrence and significance of gneissic amphibolites in the Vema fracture zone, equatorial Mid-Atlantic Ridge / Geological Society, London, Special Publications, 13:121-130, doi:10.1144/GSL.SP.1984.013.01.11 --- J. A. Karson: Variations in structure and petrology in the Coastal Complex, Newfoundland: anatomy of an oceanic fracture zone / Geological Society, London, Special Publications, 13:131-144, doi:10.1144/GSL.SP.1984.013.01.12 --- Mantle Structures --- A. Nicolas and M. Rabinowicz: Mantle flow pattern at oceanic spreading centres: relation with ophiolitic and oceanic structures / Geological Society, London, Special Publications, 13:147-151, doi:10.1144/GSL.SP.1984.013.01.13 --- Lavas and Sediments --- J. Malpas and G. Langdon: Petrology of the Upper Pillow Lava suite, Troodos ophiolite, Cyprus / Geological Society, London, Special Publications, 13:155-167, doi:10.1144/GSL.SP.1984.013.01.14 --- J. F. Boyle and A. H. F. Robertson: Evolving metallogenesis at the Troodos spreading axis / Geological Society, London, Special Publications, 13:169-181, doi:10.1144/GSL.SP.1984.013.01.1--- Isotope Studies & Metamorphism --- D. Elthon, J. R. Lawrence, R. E. Hanson, and C. Stern: Modelling of oxygen-isotope data from the Sarmiento ophiolite complex, Chile / Geological Society, London, Special Publications, 13:185-197, doi:10.1144/GSL.SP.1984.013.01.16 --- D. S. Stakes, H. P. Taylor , jr, and R. L. Fisher: Oxygen-isotope and geochemical characterization of hydrothermal alteration in ophiolite complexes and modern oceanic crust / Geological Society, London, Special Publications, 13:199-214, doi:10.1144/GSL.SP.1984.013.01.17 --- M. J. Thirlwall and B. J. Bluck: Sr-Nd isotope and chemical evidence that the Ballantrae ‘ophiolite’, SW Scotland, is polygenetic / Geological Society, London, Special Publications, 13:215-230, doi:10.1144/GSL.SP.1984.013.01.18 --- M. A. Menzies: Chemical and isotopic heterogeneities in orogenic and ophiolitic peridotites / Geological Society, London, Special Publications, 13:231-240, doi:10.1144/GSL.SP.1984.013.01.19 --- Zulfiqar Ahmed and A. Hall: Petrology and mineralization of the Sakhakot-Qila ophiolite, Pakistan / Geological Society, London, Special Publications, 13:241-252, doi:10.1144/GSL.SP.1984.013.01.20 --- II. Emplacement (Obduction) of Ophiolites --- Ophiolite Emplacement and Obduction --- J. G. Spray: Possible causes and consequences of upper mantle decoupling and ophiolite displacement / Geological Society, London, Special Publications, 13:255-268, doi:10.1144/GSL.SP.1984.013.01.21 --- J. F. Casey and J. F Dewey: Initiation of subduction zones along transform and accreting plate boundaries, triple-junction evolution, and forearc spreading centres—implications for ophiolitic geology and obduction / Geological Society, London, Special Publications, 13:269-290, doi:10.1144/GSL.SP.1984.013.01.22 --- Y. Ogawa and J. Naka: Emplacement of ophiolitic rocks in forearc areas: Examples from central Japan and Izu-Mariana-Yap island arc system / Geological Society, London, Special Publications, 13:291-301, doi:10.1144/GSL.SP.1984.013.01.23 --- M. P. Searle and R. K. Stevens: Obduction processes in ancient, modern and future ophiolites / Geological Society, London, Special Publications, 13:303-319, doi:10.1144/GSL.SP.1984.013.01.24 --- N. H. Woodcock and A. H. F. Robertson: The structural variety in Tethyan ophiolite terrains / Geological Society, London, Special Publications, 13:321-330, doi:10.1144/GSL.SP.1984.013.01.25 --- Regional Studies --- H. Colley: An ophiolite suite in Fiji? / Geological Society, London, Special Publications, 13:333-340, doi:10.1144/GSL.SP.1984.013.01.26 --- H. L. Davies and A. L. Jaques: Emplacement of ophiolite in Papua New Guinea / Geological Society, London, Special Publications, 13:341-349, doi:10.1144/GSL.SP.1984.013.01.27 --- J. S. Milsom: The gravity field of the Marum ophiolite complex, Papua New Guinea / Geological Society, London, Special Publications, 13:351-357, doi:10.1144/GSL.SP.1984.013.01.28 --- R. G. Coleman: Ophiolites and the tectonic evolution of the Arabian Peninsula / Geological Society, London, Special Publications, 13:359-366, doi:10.1144/GSL.SP.1984.013.01.29 --- G. Wadge, G. Draper, and J. F. Lewis: Ophiolites of the northern Caribbean: A reappraisal of their roles in the evolution of the Caribbean plate boundary / Geological Society, London, Special Publications, 13:367-380, doi:10.1144/GSL.SP.1984.013.01.30 --- B. A. Sturt, H. Furnes, and D. Roberts: A conspectus of Scandinavian Caledonian ophiolites / Geological Society, London, Special Publications, 13:381-391, doi:10.1144/GSL.SP.1984.013.01.31 --- R. Hall: Ophiolites: Figments of Oceanic Lithosphere? / Geological Society, London, Special Publications, 13:393-403, doi:10.1144/GSL.SP.1984.013.01.32 --- D. A. Rothery: The role of Landsat Multispectral Scanner (MSS) imagery in mapping the Oman ophiolite / Geological Society, London, Special Publications, 13:405-413, doi:10.1144/GSL.SP.1984.013.01.33
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    Amsterdam [u.a.] : Elsevier
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    Call number: 10/M 02.0598
    In: Developments in geochemistry
    Type of Medium: Monograph available for loan
    Pages: xvii, 226 S.
    Edition: 1st ed.
    ISBN: 0444505695
    Series Statement: Developments in geochemistry 7
    Classification:
    Geochemistry
    Language: English
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  • 86
    GFZ publications
    GFZ publications
    Potsdam : GeoForschungsZentrum
    Associated volumes
    Call number: 21/STR 02/13
    In: Scientific technical report
    Description / Table of Contents: Chandler and annual wobbles based on space-geodetic measurements: In this study, we examine the major components of polar motion, focusing on quantifying their temporal variability. In particular, by using the combined Earth orientation series SPACE99 computed by the Jet Propulsion Laboratory (JPL) from 1976 to 2000 at daily intervals, the Chandler and annual wobbles are separated by recursive band-pass filtering of the ?1- and ?2 -components. Then, for the trigonometric, exponential, and elliptic forms of representation,the parameters including their uncertainties are computed at epochs using quarterly sampling. The characteristics and temporal evolution of the wobbles are presented, as well as a summary of estimates of different parameters for four epochs.
    Description / Table of Contents: Polar motions with a half-Chandler period and less in their temporal variability: Our study focuses on the observed higher-frequency polar motions that are substantially smaller than the Chandler and annual wobbles. Here, the combined Earth orientation series SPACE99 from 1976 to 2000 with one-day sampling is used as input data, after removing the low-frequency, the Chandler and annual terms. We applied a dataprocessing procedure including four steps, each computing the amplitude spectrum by a Fast Fourier Transform in order to reveal the periodic signals in the residual motions, and then separating their components from the residual time series by band-pass filtering. In particular, the oscillations have the following periods: Semi-Chandler and semi-annual periods and those of order four, three, two, and one and a half months, as well as quasi-biennial and 300-day periods. We show to what extent the observed polar motions are irregularly occurring. A very small polar motion signal with the period ofone month is still found in the remaining motions.
    Type of Medium: GFZ publications
    Pages: 23 S.
    Series Statement: Scientific technical report / Geoforschungszentrum Potsdam 02/13
    Classification:
    Geodynamics
    Language: English
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  • 87
    Call number: 9/G 9207
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 322 S. , Ill., graph. Darst., Kt.
    ISBN: 0632010738
    Series Statement: Geological Society special publication 16
    Language: English
    Note: Processes --- Richard V. Fisher: Submarine volcaniclastic rocks / Geological Society, London, Special Publications, 16:5-27, doi:10.1144/GSL.SP.1984.016.01.02 --- Eizo Yamada: Subaqueous pyroclastic flows: their development and their deposits / Geological Society, London, Special Publications, 16:29-35, doi:10.1144/GSL.SP.1984.016.01.03 --- Steven Carey and Haraldur Sigurdsson: A model of volcanogenic sedimentation in marginal basins / Geological Society, London, Special Publications, 16:37-58, doi:10.1144/GSL.SP.1984.016.01.04 --- Andrew D. Saunders and John Tarney: Geochemical characteristics of basaltic volcanism within back-arc basins / Geological Society, London, Special Publications, 16:59-76, doi:10.1144/GSL.SP.1984.016.01.05 --- J. A. Pearce, S. J. Lippard, and S. Roberts: Characteristics and tectonic significance of supra-subduction zone ophiolites / Geological Society, London, Special Publications, 16:77-94, doi:10.1144/GSL.SP.1984.016.01.06 --- Western Pacific Region --- E. C. Leitch: Marginal basins of the SW Pacific and the preservation and recognition of their ancient analogues: a review / Geological Society, London, Special Publications, 16:97-108, doi:10.1144/GSL.SP.1984.016.01.07 --- J. W. Cole: Taupo-Rotorua Depression: an ensialic marginal basin of North Island, New Zealand / Geological Society, London, Special Publications, 16:109-120, doi:10.1144/GSL.SP.1984.016.01.08 --- K. B. Lewis and H. M. Pantin: Intersection of a marginal basin with a continent: structure and sediments of the Bay of Plenty, New Zealand / Geological Society, London, Special Publications, 16:121-135, doi:10.1144/GSL.SP.1984.016.01.09 --- D. S. Cronan, R. Hodkinson, S. A. Moorby, G. P. Glasby, K. Knedler, and J. Thomson: Hydrothermal and volcaniclastic sedimentation on the Tonga-Kermadec Ridge and in its adjacent marginal basins / Geological Society, London, Special Publications, 16:137-149, doi:10.1144/GSL.SP.1984.016.01.10 --- H. Colley and W. H. Hindle: Volcano-tectonic evolution of Fiji and adjoining marginal basins / Geological Society, London, Special Publications, 16:151-162, doi:10.1144/GSL.SP.1984.016.01.11 --- I. E. Smith and J. S. Milsom: Late Cenozoic volcanism and extension in Eastern Papua / Geological Society, London, Special Publications, 16:163-171, doi:10.1144/GSL.SP.1984.016.01.12 --- P. M. Sychev and A. Y. Sharaskin: Heat flow and magmatism in the NW Pacific back-arc basins / Geological Society, London, Special Publications, 16:173-181, doi:10.1144/GSL.SP.1984.016.01.13 --- South America & Antarctica --- G. Åberg, L. Aguirre, B. Levi, J. O. Nyström, and L. Aguirre: Spreading-subsidence and generation of ensialic marginal basins: an example from the early Cretaceous of central Chile / Geological Society, London, Special Publications, 16:185-193, doi:10.1144/GSL.SP.1984.016.01.14 --- D. S. Bartholomew and J. Tarney: Crustal extension in the Southern Andes (45–46°S) / Geological Society, London, Special Publications, 16:195-205, doi:10.1144/GSL.SP.1984.016.01.15 --- B. C. Storey and D. I. M. Macdonald: Processes of formation and filling of a Mesozoic back-arc basin on the island of South Georgia / Geological Society, London, Special Publications, 16:207-218, doi:10.1144/GSL.SP.1984.016.01.16 --- G. W. Farquharson, R. D. Hamer, and J. R. Ineson: Proximal volcaniclastic sedimentation in a Cretaceous back-arc basin, northern Antarctic Peninsula / Geological Society, London, Special Publications, 16:219-229, doi:10.1144/GSL.SP.1984.016.01.17 --- Lower Palaeozoic --- D. Roberts, T. Grenne, and P. D. Ryan: Ordovician marginal basin development in the central Norwegian Caledonides / Geological Society, London, Special Publications, 16:233-244, doi:10.1144/GSL.SP.1984.016.01.18 --- B. P. Kokelaar, M. F. Howells, R. E. Bevins, R. A. Roach, and P. N. Dunkley: The Ordovician marginal basin of Wales / Geological Society, London, Special Publications, 16:245-269, doi:10.1144/GSL.SP.1984.016.01.19 --- B. E. Lorenz: Mud-magma interactions in the Dunnage Mélange, Newfoundland / Geological Society, London, Special Publications, 16:271-277, doi:10.1144/GSL.SP.1984.016.01.20 --- Guoqiang Pan: The Late Precambrian and early Palaeozoic marginal basin of South China / Geological Society, London, Special Publications, 16:279-284, doi:10.1144/GSL.SP.1984.016.01.21 --- Zhijin Zhang: Lower Palaeozoic volcanism of northern Qilianshan, NW China / Geological Society, London, Special Publications, 16:285-289, doi:10.1144/GSL.SP.1984.016.01.22 --- B. P. Kokelaar, M. F. Howells, R. E. Bevins, and R. A. Roach: Volcanic and associated sedimentary and tectonic processes in the Ordovician marginal basin of Wales: a field guide / Geological Society, London, Special Publications, 16:291-322, doi:10.1144/GSL.SP.1984.016.01.23
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  • 88
    Call number: NBM 02.0555
    Type of Medium: Non-book medium
    Pages: 1 CD-ROM
    Classification:
    Informatics
    Language: English
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  • 89
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/G 9173
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 413 S.
    Series Statement: Developments in sedimentology 9b
    Language: English
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  • 90
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: 5/12208
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: xiii, 754 S.
    ISBN: 0875900208
    Series Statement: Geophysical monograph 20
    Language: English
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  • 91
    Monograph available for loan
    Monograph available for loan
    Lisse [u.a.] : Balkema
    Call number: 5/M 03.0164
    Type of Medium: Monograph available for loan
    Pages: xiii, 221 S.
    ISBN: 9058092208
    Uniform Title: Géodynamique
    Classification:
    Geophysics
    Language: English
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  • 92
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0059
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: This book has been several years in the making, under the experienced and careful oversight of Ed Grew (University of Maine), who edited (with Larry Anovitz) a similar, even larger volume in 1996: Boron: Mineralogy, Petrology, and Geochemistry (RiMG Vol. 33, reprinted with updates and corrections, 2002). Many of the same reasons for inviting investigators to contribute to a volume on B apply equally to a volume on Be. Like B, Be poses analytical difficulties, and it has been neglected in many studies. However, with recent improvements in analytical technology, interest in Be and its cosmogenic isotopes has increased greatly. Chapter 1 (Grew) is an overview of Be studies in the earth sciences backed by an extensive reference list, and an annotated list of the 110 mineral species reported to contain essential Be as of 2002, together with commentary on their status. A systematic classification of Be minerals based on their crystal structure is presented in Chapter 9 (Hawthorne and Huminicki), while analysis of these minerals by the secondary ion mass spectroscopy is the subject of Chapter 8 (Hervig). Chapter 13 (Franz and Morteani) reviews experimental studies of systems involving Be. Chapter 2 (Shearer) reviews the behavior of Be in the Solar System, with an emphasis on meteorites, the Moon and Mars, and the implications of this behavior for the evolution of the solar system. Chapter 3 (Ryan) is an overview of the terrestrial geochemistry of Be, and Chapter 7 (Vesely, Norton, Skrivan, Majer, Kr·m, Navr·til, and Kaste) discusses the contamination of the environment by this anthropogenic toxin. The cosmogenic isotopes Be-7 and Be-10 have found increasing applications in the Earth sciences. Chapter 4 (Bierman, Caffee, Davis, Marsella, Pavich, Colgan and Mickelson) reports use of the longer lived Be-10 to assess erosion rates and other surficial processes, while Chapter 5 (Morris, Gosse, Brachfeld and Tera) considers how this isotope can yield independent temporal records of geomagnetic field variations for comparison with records obtained by measuring natural remnant magnetization, be a chemical tracer for processes in convergent margins, and can date events in Cenozoic tectonics. Chapter 6 (Kaste, Norton and Hess) reviews applications of the shorter lived isotope Be-7 in environmental studies. Beryllium is a lithophile element concentrated in the residual phases of magmatic systems. Residual phases include acidic plutonic and volcanic rocks, whose geochemistry and evolution are covered, respectively, in Chapters 11 (London and Evensen) and 14 (Barton and Young), while granitic pegmatites, which are well-known for their remarkable, if localized, Be enrichments and a wide variety of Be mineral assemblages, are reviewed in Chapter 10 (Cerny). Not all Be concentrations have obvious magmatic affinities; for example, one class of emerald deposits results from Be being introduced by heated brines (Chapters 13; 14). Pelitic rocks are an important reservoir of Be in the Earth's crust and their metamorphism plays a critical role in recycling of Be in subduction zones (Chapter 3), eventually, anatectic processes complete the cycle, providing a source of Be for granitic rocks (Chapters 11 and 12).
    Type of Medium: Monograph available for loan
    Pages: XII, 691 S.
    ISBN: 0-939950-62-6 , 978-0-939950-62-1
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 50
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. Mineralogy, Petrology and Geochemistry of Beryllium: An Introduction and List of Beryllium Minerals by Edward S. Grew, p. 1 - 76 Chapter 2. Behavior of Beryllium During Solar System and Planetary Evolution: Evidence from Planetary Materials by Charles K. Shearer, p. 77 - 120 Chapter 3. Trace-Element Systematics of Beryllium in Terrestrial Materials by Jeffrey G. Ryan, p. 121 - 146 Chapter 4. Rates and Timing of Earth Surface Processes From In Situ-Produced Cosmogenic Be-10 by Paul R. Bierman, Marc W. Caffee, P. Thompson Davis, Kim Marsella, Milan Pavich, Patrick Colgan, and David Mickelson, p. 147 - 206 Chapter 5. Cosmogenic Be-10 and the Solid Earth: Studies in Geomagnetism, Subduction Zone Processes, and Active Tectonics by Julie D. Morris, John Gosse, Stefanie Brachfeld, and Fouad Tera, p. 207 - 270 Chapter 6. Environmental Chemistry of Beryllium-7 by James M. Kaste, Stephen A. Norton, and Charles T. Hess, p. 271 - 290 Chapter 7. Environmental Chemistry of Beryllium by J. Vesely, S. A. Norton, P. Skrivan, V. Majer, P. Kram, T. Navr·til, and J. M. Kaste, p. 291 - 318 Chapter 8. Beryllium Analyses by Secondary Ion Mass Spectrometry by Richard L. Hervig, p. 319 - 332 Chapter 9. The Crystal Chemistry of Beryllium by Frank C. Hawthorne and Danielle M. C. Huminicki, p. 333 - 404 Chapter 10. Mineralogy of Beryllium in Granitic Pegmatites by Petr Cerny, p. 405 - 444 Chapter 11. Beryllium in Silicic Magmas and the Origin of Beryl-Bearing Pegmatites by David London and Joseph M. Evensen, p. 445 - 486 Chapter 12. Beryllium in Metamorphic Environments (Emphasis on Aluminous Compositions) by Edward S. Grew, p. 487 - 550 Chapter 13. Be-Minerals: Synthesis, Stability, and Occurrence in Metamorphic Rocks by Gerhard Franz and Giulio Morteani, p. 551 - 590 Chapter 14. Non-pegmatitic Deposits of Beryllium: Mineralogy, Geology, Phase Equilibria and Origin by Mark D. Barton and Steven Young, p. 591 - 691
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  • 93
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(D-59) / Mag. 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 86 S.
    ISBN: 8388765213
    Series Statement: Publications of the Institute of Geophysics, Polish Akademy of Sciences : D, Physics of the atmosphere 59 = 349
    Language: English
    Location: Magazine - must be ordered
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  • 94
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(B-27) / Mag. 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 180 S.
    ISBN: 8388765116
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 27 = 339 : monographic volume
    Classification:
    Seismology
    Language: English
    Location: Magazine - must be ordered
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  • 95
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Pr.
    Call number: 5/M 03.0198 ; 5/M 03.0307 ; 21/M 04.0258
    Type of Medium: Monograph available for loan
    Pages: xxiv, 471 S.
    Edition: 2nd ed.
    ISBN: 0521655404
    Classification:
    Seismology
    Language: English
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  • 96
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Associated volumes
    Call number: 5/M 03.0184 ; M 04.0033
    In: The seismic wavefield
    Type of Medium: Monograph available for loan
    Pages: xii, 534 S.
    ISBN: 0521006651
    Language: English
    Location: Reading room
    Location: Upper compact magazine
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  • 97
    Series available for loan
    Series available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0180
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Exactly 100 years before the publication of this volume, the first paper which calculated the half-life for the newly discovered radioactive substance U-X (now called 234Th), was published. Now, in this volume, the editors Bernard Bourdon, Gideon Henderson, Craig Lundstrom and Simon Turner have integrated a group of contributors who update our knowledge of U-series geochemistry, offer an opportunity for non-specialists to understand its basic principles, and give us a view of the future of this active field of research. In this volume, for the first time, all the methods for determining the uranium and thorium decay chain nuclides in Earth materials are discussed. It was prepared in advance of a two-day short course (April 3-4, 2003) on U-series geochemistry, jointly sponsored by GS and MSA and presented in Paris, France prior to the joint EGS/AGU/EUG meeting in Nice. The discovery of the 238U decay chain, of course, started with the seminal work of Marie Curie in identifying and separating 226Ra. Through the work of the Curies and others, all the members of the 238U decay chain were identified. An important milestone for geochronometrists was the discovery of 230Th (called Ionium) by Bertram Boltwood, the Yale scientist who also made the first age determinations on minerals using the U-Pb dating method (Boltwood in 1906 established the antiquity of rocks and even identified a mineral from Sri Lanka-then Ceylon as having an age of 2.1 billion years!) The application of the 238U decay chain to the dating of deep sea sediments was by Piggott and Urry in 1942 using the "Ionium" method of dating. Actually they measured 222Ra (itself through 222Rn) assuming secular equilibrium had been established between 230Th and 226Ra. Although 230Th was measured in deep sea sediments by Picciotto and Gilvain in 1954 using photographic emulsions, it was not until alpha spectrometry was developed in the late 1950's that 20Th was routinely measured in marine deposits. Alpha spectrometry and gamma spectrometry became the work horses for the study of the uranium and thorium decay chains in a variety of Earth materials. These ranged from 222Rn and its daughters in the atmosphere, to the uranium decay chain nuclides in the oceanic water column, and volcanic rocks and many other systems in which either chronometry or element partitioning, were explored. Much of what we learned about the 238U, 235U and 232Th decay chain nuclides as chronometers and process indicators we owe to these seminal studies based on the measurement of radioactivity. The discovery that mass spectrometry would soon usurp many of the tasks performed by radioactive counting was in itself serendipitous. It came about because a fundamental issue in cosmochemistry was at stake. Although variation in 235U/238U had been reported for meteorites the results were easily discredited as due to analytical difficulties. One set of results, however, was published by a credible laboratory long involved in quality measurements of high mass isotopes such as the lead isotopes. The purported discovery of 235U/238U variations in meteorites, if true, would have consequences in defining the early history of the formation of the elements and the development of inhomogeneity of uranium isotopes in the accumulation of the protoplanetary materials of the Solar System. Clearly the result was too important to escape the scrutiny of falsification implicit in the way we do science. The Lunatic Asylum at Caltech under the leadership of Jerry Wasserburg took on that task. Jerry Wasserburg and Jim Chen clearly established the constancy and Earth-likeness of 235U/238U in the samplable universe. In the hands of another member of the Lunatic Asylum, Larry Edwards, the methodology was transformed into a tool for the study of the 238U decay chain in marine systems. Thus the mass spectrometric techniques developed provided an approach to measuring the U and Th isotopes in geological materials as well as cosmic materials with the same refinement and accommodation for small sample size. Soon after this discovery the harnessing of the technique to the measurement of all the U isotopes and all the Th isotopes with great precision immediately opened up the entire field of uranium and thorium decay chain studies. This area of study was formerly the poaching ground for radioactive measurements alone but now became part of the wonderful world of mass spectrometric measurements. (The same transformation took place for radiocarbon from the various radioactive counting schemes to 'accelerator mass spectrometry.) No Earth material was protected from this assault. The refinement of dating corals, analyzing volcanic rocks for partitioning and chronometer studies and extensions far and wide into ground waters and ocean bottom dwelling organisms has been the consequence of this innovation. Although Ra isotopes, 210Pb and 210Po remain an active pursuit of those doing radioactive measurements, many of these nuclides have also become subject to the mass spectrometric approach. In this volume, for the first time, all the methods for determining the uranium and thorium decay chain nuclides in Earth materials are discussed. The range of problems solvable with this approach is remarkable-a fitting, tribute to the Curies and the early workers who discovered them for us to use.
    Type of Medium: Series available for loan
    Pages: xx, 656 S.
    ISBN: 0-939950-64-2 , 978-0-939950-64-5
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 52
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. Introduction to U-series Geochemistry by Bernard Bourdon, Simon Turner, Gideon M. Henderson and Craig C. Lundstrom, p. 1 - 22 Chapter 2. Techniques for Measuring Uranium-series Nuclides: 1992-2002 by Steven J. Goldstein and Claudine H. Stirling, p. 23 - 58 Chapter 3. Mineral-Melt Partitioning of Uranium, Thorium and Their Daughters by Jonathan Blundy and Bernard Wood, p. 59 - 124 Chapter 4. Timescales of Magma Chamber Processes and Dating of Young Volcanic Rocks by Michel Condomines, Pierre-Jean Gauthier, and Olgeir Sigmarsson, p. 125 - 174 Chapter 5. Uranium-series Disequilibria in Mid-ocean Ridge Basalts: Observations and Models of Basalt Genesis by Craig C. Lundstrom, p. 175 - 214 Chapter 6. U-series Constraints on Intraplate Basaltic Magmatism by Bernard Bourdon and Kenneth W. W. Sims, p. 215 - 254 Chapter 7. Insights into Magma Genesis at Convergent Margins from U-series Isotopes by Simon Turner, Bernard Bourdon and Jim Gill, p. 255 - 316 Chapter 8. The Behavior of U- and Th-series Nuclides in Groundwater by Donald Porcelli and Peter W. Swarzenski, p. 317 - 362 Chapter 9. Uranium-series Dating of Marine and Lacustrine Carbonates by R. L. Edwards, C. D. Gallup, and H. Cheng, p. 363 - 406 Chapter 10. Uranium-series Chronology and Environmental Applications of Speleothems by David A. Richards and Jeffrey A. Dorale, p. 407 - 460 Chapter 11. Short-lived U/Th Series Radionuclides in the Ocean: Tracers for Scavenging Rates, Export Fluxes and Particle Dynamics by J. K. Cochran and P. Masquè, p. 461 - 492 Chapter 12. The U-series Toolbox for Paleoceanography by Gideon M. Henderson and Robert F. Anderson, p. 493 - 532 Chapter 13. U-Th-Ra Fractionation During Weathering and River Transport by F. Chabaux, J. Riotte and O. Dequincey, p. 533 - 576 Chapter 14. The Behavior of U- and Th-series Nuclides in the Estuarine Environment by Peter W. Swarzenski, Donald Porcelli, Per S. Andersson and Joseph M. Smoakv, p. 577 - 606 Chapter 15. U-series Dating and Human Evolution by A. W. G. Pike and P. B. Pettitt, p. 607 - 630 Chapter 16. Mathematical-Statistical Treatment of Data and Errors for 230Th/U Geochronology by K. R. Ludwig, p. 631 - 656
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  • 98
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0179
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: This volume highlights some of the frontiers in the study of plastic deformation of minerals and rocks. The research into the plastic properties of minerals and rocks had a major peak in late 1960s to early 1970s, largely stimulated by research in the laboratory of D. T. Griggs and his students and associates. It is the same time when the theory of plate tectonics was established and provided a first quantitative theoretical framework for understanding geological processes. The theory of plate tectonics stimulated the study of deformation properties of Earth materials, both in the brittle and the ductile regimes. Many of the foundations of plastic deformation of minerals and rocks were established during this period. Also, new experimental techniques were developed, including deformation apparatus for high-pressure and high-temperature conditions, electron micros-copy study of defects in minerals, and the X-ray technique of deformation fabric analysis. The field benefited greatly from materials science concepts of deformation that were introduced, including the models of point defects and their interaction with dislocations. A summary of progress is given by the volume Flow and Fracture of Rocks: The Griggs Volume, published in 1972 by the American Geophysical Union. Since then, the scope of Earth sciences has greatly expanded. Geodynamics became concerned with the Earth's deep interior where seismologists discovered heterogeneities and anisotropy at all scales that were previously thought to be typical of the crust and the upper mantle. Investigations of the solar system documented new mineral phases and rocks far beyond the Earth. Both domains have received a lot of attention from mineralogists (e.g., summarized in MSA's Reviews in Mineralogy, Volume 36, Planetary Materials and Volume 37, Ultra-High Pressure Mineralogy). Most attention was directed towards crystal chemistry and phase relations, yet an understanding of the deformation behavior is essential for interpreting the dynamic geological processes from geological and geophysical observations. This was largely the reason for a rebirth of the study of rock plasticity, leading to new approaches that include experiments at extreme conditions and modeling of deformation behavior based on physical principles. A wide spectrum of communities emerged that need to use information about mineral plasticity, including mineralogy, petrology, structural geology, seismology, geodynamics and engineering. This was the motivation to organize a workshop, in December 2002 in Emeryville, California, to bridge the very diverse disciplines and facilitate communication. This volume written for this workshop should help one to become familiar with a notoriously difficult subject, and the various contributions represent some of the important progress that has been achieved. The spectrum is broad. High-resolution tomographic images of Earth's interior obtained from seismology need to be interpreted on the bases of materials properties to understand their geodynamic significance. Key issues include the influence of deformation on seismic signatures, such as attenuation and anisotropy, and a new generation of experimental and theoretical studies on rock plasticity has contributed to a better understanding. Extensive space exploration has revealed a variety of tectonic styles on planets and their satellites, underlining the uniqueness of the Earth. To understand why plate tectonics is unique to Earth, one needs to understand the physical mechanisms of localization of deformation at various scales and under different physical conditions. Also here important theoretical and experimental studies have been conducted. In both fields, studies on anisotropy and shear localization, large-strain deformation experiments and quantitative modeling are critical, and these have become available only recently. Complicated interplay among chemical reactions (including partial melting) is a key to understand the evolution of Earth. This book contains two chapters on the developments of new techniques of experimental studies: one is large-strain shear deformation (Chapter 1 by Mackwell and Paterson) and another is deformation experiments under ultrahigh pressures (Chapter 2 by Durham et al.). Both technical developments are the results of years of efforts that are opening up new avenues of research along which rich new results are expected to be obtained. Details of physical and chemical processes of deformation in the crust and the upper mantle are much better understood through the combination of well controlled laboratory experiments with observations on "real" rocks deformed in Earth. Chapter 3 by Tullis and Chapter 4 by Hirth address the issues of deformation of crustal rocks and the upper mantle, respectively. In Chapter 5 Kohlstedt reviews the interplay of partial melting and deformation, an important subject in understanding the chemical evolution of Earth. Cordier presents in Chapter 6 an overview of the new results of ultrahigh pressure deformation of deep mantle minerals and discusses microscopic mechanisms controlling the variation of deformation mechanisms with minerals in the deep mantle. Green and Marone review in Chapter 7 the stability of deformation under deep mantle conditions with special reference to phase transformations and their relationship to the origin of intermediate depth and deep-focus earthquakes. In Chapter 8 Schulson provides a detailed description of fracture mechanisms of ice, including the critical brittle-ductile transition that is relevant not only for glaciology, planetology and engineering, but for structural geology as well. In Chapter 9 Cooper provides a review of experimental and theoretical studies on seismic wave attenuation, which is a critical element in interpreting distribution of seismic wave velocities and attenuation. Chapter 10 by Wenk reviews the relationship between crystal preferred orientation and macroscopic anisotropy, illustrating it with case studies. In Chapter 11 Dawson presents recent progress in poly-crystal plasticity to model the development of anisotropic fabrics both at the microscopic and macroscopic scale. Such studies form the basis for geodynamic interpretation of seismic anisotropy. Finally, in Chapter 12 Montagner and Guillot present a thorough review of seismic anisotropy of the upper mantle covering the vast regions of geodynamic interests, using a global surface wave data set. In Chapter 13 Bercovici and Karato summarize the theoretical aspects of shear localization. All chapters contain extensive reference lists to guide readers to the more specialized literature. Obviously this book does not cover all the areas related to plastic deformation of minerals and rocks. Important topics that are not fully covered in this book include mechanisms of semi-brittle deformation and the interplay between microstructure evolution and deformation at different levels, such as dislocation substructures and grain-size evolution ("self-organization"). However, we hope that this volume provides a good introduction for graduate students in Earth science or materials science as well as the researchers in these areas to enter this multidisciplinary field.
    Type of Medium: Monograph available for loan
    Pages: xii, 420 S..
    ISBN: 0-939950-63-4 , 978-0-939950-63-8
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 51
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. New Developments in Deformation Studies: High-Strain Deformation by Stephen J. Mackwell and Mervyn S. Paterson, p. 1 - 20 Chapter 2. New Developments in Deformation Experiments at High Pressure by William B. Durham, Donald J. Weidner, Shun-ichiro Karato, and Yanbin Wang, p. 21 - 50 Chapter 3. Deformation of Granitic Rocks: Experimental Studies and Natural Examples by Jan Tullis, p. 51 - 96 Chapter 4. Laboratory Constraints on the Rheology of the Upper Mantle by Greg Hirth, p. 97 - 120 Chapter 5. Partial Melting and Deformation by David L. Kohlstedt, p. 121 - 136 Chapter 6. Dislocations and Slip Systems of Mantle Minerals by Patrick Cordier, p. 137 - 180 Chapter 7. Instability of Deformation by Harry W. Green II and Chris Marone, p. 181 - 200 Chapter 8. Brittle Failure of Ice by Erland M. Schulson, p. 201 - 525 Chapter 9. Seismic Wave Attenuation: Energy Dissipation in Viscoelastic Crystalline Solids by Reid F. Cooper, p. 253 - 290 Chapter 10. Texture and Anisotropy by Hans-Rudolf Wenk, p. 291 - 330 Chapter 11. Modeling Deformation of Polycrystalline Rocks by Paul R. Dawson, p. 331 - 352 Chapter 12. Seismic Anisotropy and Global Geodynamics by Jean-Paul Montagner and Laurent Guillot, p. 353 - 386 Chapter 13. Theoretical Analysis of Shear Localization in the Lithosphere by David Bercovici and Shun-ichiro Karato, p. 387 - 420
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    Call number: 21/SR 90.0917(41-42) ; MOP 40703 / Mitte
    In: Veröffentlichungen des Zentralinstituts für Physik der Erde
    Type of Medium: Series available for loan
    Pages: 201 S.
    Edition: Als Ms. gedr.
    Series Statement: Veröffentlichungen des Zentralinstituts für Physik der Erde 41
    Language: English
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    Call number: 21/SR 90.0917(78)
    Type of Medium: Series available for loan
    Pages: 172 S.
    Edition: Als Ms. gedr.
    Series Statement: Veröffentlichungen des Zentralinstituts für Physik der Erde 78
    Language: English
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