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  • Books  (42)
  • Tectonics  (19)
  • Geochemistry  (18)
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  • 1
    Call number: 9/M 07.0421(468)
    In: Geological Society Special Publication
    Type of Medium: Monograph available for loan
    Pages: 208 Seiten , Diagramme
    ISBN: 978-1-78620-366-3
    Series Statement: Geological Society Special Publication 468
    Classification:
    Geochemistry
    Language: English
    Note: Hydrocarbon systems, by nature, are a complex interplay of elements that must be spatially and temporally aligned to result in the generation and preservation of subsurface hydrocarbon accumulations. To meet the increasing challenges of discovering hydrocarbon resources, it is essential that we advance our understanding of these systems through new geochemical approaches and analytical developments. Such development requires that academic- and industry-led research efforts converge in ways that are unique to the geosciences. The aim of this volume is to bring together a multidisciplinary geochemical community from industry and academia working in hydrocarbon systems to publish recent advances and state-of-the-art approaches to resolve the many remaining questions in hydrocarbon systems analysis. From Source to Seep presents geochemical and isotopic studies that are grouped into three themes: (1) source-rock identification and the temperature/timing of hydrocarbon generation; (2) mechanisms and time-scales associated with hydrocarbon migration, trapping, storage and alteration; and (3) the impact of fluid flow on reservoir properties. | Contents: Geochemical applications in petroleum systems analysis: new constraints and the power of integration / M. Lawson, M. J. Formolo, L. Summa and J. M. Eiler / Geological Society, London, Special Publications, 468, 1-21, 19 February 2018, https://doi.org/10.1144/SP468.6 --- Source-rock identification and the temperature/timing of hydrocarbon generation --- The utility of methane clumped isotopes to constrain the origins of methane in natural gas accumulations / Daniel A. Stolper, Michael Lawson, Michael J. Formolo, Cara L. Davis, Peter M. J. Douglas and John M. Eiler / Geological Society, London, Special Publications, 468, 23-52, 14 December 2017, https://doi.org/10.1144/SP468.3 --- The isotopic structures of geological organic compounds / John M. Eiler, Matthieu Clog, Michael Lawson, Max Lloyd, Alison Piasecki, Camilo Ponton and Hao Xie / Geological Society, London, Special Publications, 468, 53-81, 14 December 2017, https://doi.org/10.1144/SP468.4 --- Vanadium isotope composition of crude oil: effects of source, maturation and biodegradation / Yongjun Gao, John F. Casey, Luis M. Bernardo, Weihang Yang and K. K. (Adry) Bissada / Geological Society, London, Special Publications, 468, 83-103, 14 December 2017, https://doi.org/10.1144/SP468.2 --- Carbon and hydrogen isotopic compositions of n-alkanes as a tool in petroleum exploration / Nikolai Pedentchouk and Courtney Turich / Geological Society, London, Special Publications, 468, 105-125, 14 December 2017, https://doi.org/10.1144/SP468.1 --- Mechanisms and time-scales associated with hydrocarbon migration, trapping, storage and alteration --- Noble gases in conventional and unconventional petroleum systems / David J. Byrne, P. H. Barry, M. Lawson and C. J. Ballentine / Geological Society, London, Special Publications, 468, 127-149, 14 December 2017, https://doi.org/10.1144/SP468.5 --- Differentiating between biogenic and thermogenic sources of natural gas in coalbed methane reservoirs from the Illinois Basin using noble gas and hydrocarbon geochemistry / Myles T. Moore, David S. Vinson, Colin J. Whyte, William K. Eymold, Talor B. Walsh and Thomas H. Darrah / Geological Society, London, Special Publications, 468, 151-188, 18 January 2018, https://doi.org/10.1144/SP468.8 --- The impact of fluid flow on reservoir properties --- Testing clumped isotopes as a reservoir characterization tool: a comparison with fluid inclusions in a dolomitized sedimentary carbonate reservoir buried to 2–4 km / John M. MacDonald, Cédric M. John and Jean-Pierre Girard / Geological Society, London, Special Publications, 468, 189-202, 14 December 2017, https://doi.org/10.1144/SP468.7
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  • 2
    Monograph available for loan
    Monograph available for loan
    Massachusetts [u.a.] : Blackwell Science
    Call number: M 94.0357
    Type of Medium: Monograph available for loan
    Pages: xi, 279 S.
    Edition: 2nd ed.
    ISBN: 0865423660
    Classification:
    Tectonics
    Language: English
    Location: Upper compact magazine
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  • 3
    Call number: 10/M 18.91518
    In: Geochemical Atlas of Europe / FOREGS
    Description / Table of Contents: The IUGS/IAGC Global Geochemical Baselines Programme aims to establish a global geochemical reference baseline for 〉60 determinants in a range of media for environmental and other applications. The European contribution to the programme has been carried out by government institutions from 26 countries under the auspices of the Forum of European Geological Surveys (FOREGS) The main objectives of this European survey were: 1) to apply standardised methods of sampling, chemical analysis and data management to prepare a geochemical baseline across Europe; and 2) to use this reference network to level national baseline datasets. Samples of stream water, stream sediment and three types of soil (organic top layer, minerogenic top and sub soil) have been collected at 900 stations, each representing a catchment area of 100 km2, corresponding to a sampling density of about one sample per 4700 km2. In addition, the uppermost 25 cm of floodplain sediment was sampled from 790 sites each representing a catchment area of 1000 km2. All soil and sediment samples were prepared at the same laboratory, and all samples of particular sample types were analysed by the same method at the same laboratory. More than 50 elements, both total and aqua regia extractable concentrations, and other parameters (such as pH and grain size) were determined on the 〈2 mm grain size fraction of minerogenic samples, and total concentrations of organic soil samples were measured after using a strong acid digestion. Nine laboratories of European geological surveys carried out the analytical work. Altogether, 360 geochemical maps showing the distribution of elements across Europe have been prepared. All the results and field observations are organised in a common database and the maps are published as a Geochemical Atlas of Europe. All the sampling sites were photographed and this photo archive is also available. Samples have been archived in the Slovak Republic for possible future use. Initial results show that the distribution patterns of both water and solid samples are related to such factors as large-scale tectonic provinces, geochemical variation of large lithological units, extension of the Weichselian glaciation, and contamination reflecting industrialized areas and regions of intensive agriculture. Key words (GeoRef Thesaurus, AGI): geochemical surveys, baseline studies, soils, sediments, stream water, sampling, sample preparation, chemical analysis, geochemical maps, atlas, areal geology, Europe
    Type of Medium: Monograph available for loan
    Pages: 526 Seiten , Illustrationen, Karten
    ISBN: 951-690-921-3
    Series Statement: Geochemical Atlas of Europe 1
    Classification:
    Geochemistry
    Language: English
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0010
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Several years ago, John Rakovan and John Hughes (colleagues at Miami of Ohio), and later Matt Kohn (at South Carolina), separately proposed short courses on phosphate minerals to the Council of the Mineralogical Society of America (MSA). Council suggested that they join forces. Thus this volume, Phosphates: Geochemical, Geobiological, and Materials Importance, was organized. It was prepared in advance of a short course of the same title, sponsored by MSA and presented at Golden, Colorado, October 25-27. We are pleased to present this volume entitled Phosphates: Geochemical, Geobiological and Materials Importance. Phosphate minerals are an integral component of geological and biological systems. They are found in virtually all rocks, are the major structural component of vertebrates, and when dissolved are critical for biological activity. This volume represents the work of many authors whose research illustrates how the unique chemical and physical behavior of phosphate minerals permits a wide range of applications that encompasses phosphate mineralogy, petrology, biomineralization, geochronology, and materials science. While diverse, these fields are all linked structurally, crystal-chemically and geochemically. As geoscientists turn their attention to the intersection of the biological, geological, and material science realms, there is no group of compounds more germane than the phosphates. The chapters of this book are grouped into five topics: Mineralogy and Crystal Chemistry, Petrology, Biomineralization, Geochronology, and Materials Applications. In the first section, three chapters are devoted to mineralogical aspects of apatite, a phase with both inorganic and organic origins, the most abundant phosphate mineral on earth, and the main mineral phase in the human body. Monazite and xenotime are highlighted in a fourth chapter, which includes their potential use as solid-state radioactive waste repositories. The Mineralogy and Crystal Chemistry section concludes with a detailed examination of the crystal chemistry of 244 other naturally-occurring phosphate phases and a listing of an additional 126 minerals. In the Petrology section, three chapters detail the igneous, metamorphic, and sedimentary aspects of phosphate minerals. A fourth chapter provides a close look at analyzing phosphates for major, minor, and trace elements using the electron microprobe. A final chapter treats the global geochemical cycling of phosphate, a topic of intense, current geochemical interest. The Biomineralization section begins with a summary of the current state of research on bone, dentin and enamel phosphates, a topic that crosses disciplines that include mineralogical, medical, and dental research. The following two chapters treat the stable isotope and trace element compositions of modern and fossil biogenic phosphates, with applications to paleontology, paleoclimatology, and paleoecology. The Geochronology section focuses principally on apatite and monazite for U-ThPb, (U- Th)/He, and fission-track age determinations; it covers both classical geochronologic techniques as well as recent developments. The final section-Materials Applications-highlights how phosphate phases play key roles in fields such as optics, luminescence, medical engineering and prosthetics, and engineering of radionuclide repositories. These chapters provide a glimpse of the use of natural phases in engineering and biomedical applications and illustrate fruitful areas of future research in geochemical, geobiological and materials science. We hope all chapters in this volume encourage researchers to expand their work on all aspects of natural and synthetic phosphate compounds.
    Type of Medium: Monograph available for loan
    Pages: xv, 742 S.
    ISBN: 0-939950-60-X , 978-0-939950-60-7
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 48
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. The Crystal Structure of Apatite, Ca5(PO4)3(F,OH,Cl) by John M. Hughes and John Rakovan, p. 1 - 12 Chapter 2. Compositions of the Apatite-Group Minerals: Substitution Mechanisms and Controlling Factors by Yuanming Pana and Michael E. Fleet, p. 13 - 50 Chapter 3. Growth and Surface Properties of Apatite by John Rakovan, p. 51 - 86 Chapter 4. Synthesis, Structure and Properties of Monazite, Pretulite, and Xenotime by Lynn A. Boatner, p. 87 - 122 Chapter 5. The Crystal Chemistry of the Phosphate Minerals by Danielle M.C. Huminicki and Frank C. Hawthorne, p. 123 - 254 Chapter 6. Apatite in Igneous Systems by Philip M. Piccoli and Philip A. Candela, p. 255 - 292 Chapter 7. Apatite, Monazite, and Xenotine in Metamorphic Rocks by Frank S. Spear and Joseph M. Pyle, p. 293 - 336 Chapter 8. Electron Microprobe Analysis of REE in Apatite, Monazite and Xenotime: Protocols and Pitfalls by Joseph M. Pyle, Frank S. Spear, and David A. Wark, p. 337 - 362 Chapter 9. Sedimentary Phosphorites - An Example: Phosphoria Formation, Southeastern Idaho, U.S.A by Andrew C. Knudsen and Mickey E. Gunter, p. 363 - 390 Chapter 10. The Global Phosphorus Cycle by Gabriel M. Filippelli, p. 391 - 426 Chapter 11. Calcium Phosphate Biominerals by James C. Elliott, p. 427 - 454 Chapter 12. Stable Isotope Composition of Biological Apatite by Matthew J. Kohn and Thure E. Cerling, p. 455 - 488 Chapter 13. Trace Elements in Recent and Fossil Bone Apatite by Clive N. Trueman and Noreen Tuross, p. 489 - 522 Chapter 14. U-TH-Pb Dating of Phosphate Minerals by T. Mark Harrison, Elizabeth J. Catlos, and Jean-Marc Montel, p. 523 - 558 Chapter 15. (U-Th)/He Dating of Phosphates: Apatite, Monazite, and Xenotime by Kenneth A. Farley and Daniel F. Stockli, p. 559 - 578 Chapter 16. Fission Track Dating of Phosphate Minerals and the Thermochronology of Apatite by Andrew J.W. Gleadow, David X. Belton, Barry P. Kohn, and Roderick W. Brown, p. 579 - 630 Chapter 17. Biomedical Application of Apatites by Karlis A. Gross and Christopher C. Berndt, p. 631 - 672 Chapter 18. Phosphates as Nuclear Waste Forms by Rodney C. Ewing and LuMin Wang, p. 673 - 700 Chapter 19. Apatite Luminescence by Glenn A. Waychuna, p. 701 - 742
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  • 5
    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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  • 6
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 04.0253
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Until only a few years ago, I would never have imagined that a volume on the stable isotope geochemistry of elements like Mg, Fe or Cu would be written. In fact, a comic book of blank pages entitled The Stable Isotope Geochemistry of Fluorine would have been a more likely prospect. In volume 16 of this series, published in 1986, I wrote: Isotopic variations have been looked for but not found for heavy elements like Cu, Sn, and Fe .... Natural variations in isotopic ratios of terrestrial materials have been reported for other light elements like Mg and K, but such variations usually turn out to be laboratory artifacts. I am about ready to eat those words. We have known for many years that large isotopic fractionations of heavy elements like Pb develop in the source regions of TIMS machines. Nonetheless, most of us held fast to the conventional wisdom that no significant mass-dependent isotopic fractionations were likely to occur in natural or laboratory systems for elements that are either heavy or engaged in bonds with a dominant ionic character. With the relatively recent appearance of new instrumentation like MC-ICP-MS and heroic methods development in TIMS analyses, it became possible to make very precise measurements of the isotopic ratios of some of these non-traditional elements, particularly if they comprise three or more isotopes. It was eminently reasonable to reexamine these systems in this new light. Perhaps atomic weights could be refined, or maybe there were some unexpected isotopic variations to discover. There were around the turn of the present century, reports began appearing of biological fractionations of about 2-3 per mil for heavy elements like Fe and Cr and attempts were made to determine the magnitude of equilibrium isotope effects in these systems, both by experiment and semi-empirical calculations. Interest emerged in applying these effects to the study of environmental problems. Even the most recalcitrant skeptic now accepts the fact that measurable and meaningful variations in the isotopic ratios of heavy elements occur as a result of chemical, biological and physical processes. Most of the work discussed in this volume was published after the year 2000 and thus the chapters are more like progress reports rather than reviews. Skepticism now focuses on whether isotopic variations as small as 0.1 per mil are indeed as meaningful as some think, and the fact that measured isotopic fractionations of these non-traditional elements are frequently much smaller than predicted from theoretical considerations. In fact the large fractionations suggested by the calculations provide much of the stimulus for working in this discipline. Clearly some carefully designed experiments could shed light on some of the ambiguity. My optimism for the future of this burgeoning new field remains high because it is in very good hands indeed. Approximately three-quarters of the elements in the Periodic Table have two or more isotopes. RiM 16 and RiMG 43 were devoted to H, C, 0, and S isotope variations, and B isotope variations were discussed in RiM 33. The importance of these elements to geochemistry may be illustrated by a GeoRef search of 0 isotope publications, which yields over 25,000 papers, theses, and abstracts spanning over five decades. Isotopic variations of the remaining 56 elements that have two or more isotopes, however, remains relatively little explored, but is gaining rapid attention, in part driven by advances in analytical instrumentation in the last 5-10 years. Our goal for this volume was to bring together a summary of the isotope geochemistry of non-traditional stable isotope systems as is known through 2003 for those elements that have been studied in some detail, and which have a variety of geochemical properties. In addition, recognizing that many of these elements are of interest to workers who are outside the traditional stable isotope fields, we felt it was important to include discussions on the broad isotopic variations that occur in the solar system, theoretical approaches to calculating isotopic fractionations, and the variety of analytical methods that are in use. We hope, therefore, that this volume proves to be useful to not only the isotope specialist, but to others who are interested in the contributions that these non-traditional stable isotopes may make toward understanding geochemical and biological cycles.
    Type of Medium: Monograph available for loan
    Pages: XV, 454 S. , Ill., graph. Darst
    ISBN: 0-939950-67-7 , 978-0-939950-67-6
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 55
    Classification:
    Geochemistry
    Note: Chapter 1. Overview and General Concepts by Clark M. Johnson, Brian L. Beard and Francis Albarede, p. 1 - 24 Chapter 2. An Overview of Isotopic Anomalies in Extraterrestrial Materials and Their Nucleosynthetic Heritage by Jean Louis Birck, p. 25 - 64 Chapter 3. Applying Stable Isotope Fractionation Theory to New Systems by Edwin A. Schauble, p. 65 - 112 Chapter 4. Analytical Methods for Non-Traditional Isotopes by Francis AlbarÀde and Brian L. Beard, p. 113 - 152 Chapter 5. Developments in the Understanding and Application of Lithium Isotopes in the Earth and Planetary Sciences by Paul B. Tomascak, p. 153 - 196 Chapter 6. The Isotope Geochemistry and Cosmochemistry of Magnesium by Edward D. Young and Albert Galy, p. 197 - 230 Chapter 7. The Stable-Chlorine Isotope Compositions of Natural and Anthropogenic Materials by Michael A. Stewart and Arthur J. Spivack, p. 231 - 254 Chapter 8. Calcium Isotopic Variations Produced by Biological, Kinetic, Radiogenic and Nucleosynthetic Processes by Donald J. DePaolo, p. 255 - 288 Chapter 9. Mass-Dependent Fractionation of Selenium and Chromium Isotopes in Low-Temperature Environments by by Thomas M. Johnson and Thomas D. Bullen, p. 289 - 318 Chapter 10A. Fe Isotope Variations in the Modern and Ancient Earth and Other Planetary Bodies by Brian L. Beard and Clark M. Johnson, p. 319 - 358 Chapter 10B. Isotopic Constraints on Biogeochemical Cycling of Fe by Clark M. Johnson, Brian L. Beard, Eric E. Roden, Dianne K. Newman and Kenneth H. Nealson, p. 359 - 408 Chapter 11. The stable isotope geochemistry of copper and zinc by Francis Albarede, p. 409 - 428 Chapter 12. Molybdenum Stable Isotopes: Observations, Interpretations and Directions by Ariel D. Anbar, p. 429 - 454
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  • 7
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Oxford Univ. Press
    Call number: 10/M 94.0701
    Type of Medium: Monograph available for loan
    Pages: xx, 588 S.
    ISBN: 019506464X
    Classification:
    Geochemistry
    Language: English
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  • 8
    Call number: 9/M 07.0421(328)
    In: Geological Society special publication
    Description / Table of Contents: This book considers the geology between North and South America. It contributes to debate about the area's evolution, particularly that of the Caribbean. Prevailing understanding is that the Caribbean formed inthe Pacific and was engulfed between the Americas as the latter drifted west. Accordingly, the CaribbeanPlate comprises internal, Jurassic-Cretaceous oceanic rocks, thickened into a Cretaceous hotspot/plumeplateau, with obducted ophiolites and Cretaceous-Palaeogene, subduction-related, intra-oceanic volcanicarc and metamorphosed arc/continental rocks exposed on its margins. An alternative interpretation is thatthe Caribbean evolved in place. It consists largely of continental crust, extended in the Triassic-Jurassic,which subsided below thick Jurassic-Cretaceous carbonate rocks and flood basalts, and Cenozoic carbonateand clastic rocks. After uplift of 'oceanic' and volcanic arc rocks onto (continental) margins, the interiorfoundered in the Middle Eocene. Papers range from regional overviews and discussions of Caribbeanorigins to aspects of local geology arranged in a circum-Caribbean tour and ending in the interior. They address tectonics, structure, geochronology, seismicity, igneous and metamorphic petrology, metamorphism, geochemistry, stratigraphy and palaeontology.
    Type of Medium: Monograph available for loan
    Pages: IX, 858 S.
    ISBN: 1862392889 , 978-1-86239-288-5
    Series Statement: Geological Society special publication 328
    Classification:
    Tectonics
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  • 9
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Freeman
    Call number: 9/M 11.0003
    Description / Table of Contents: Contents: Part I. Brittle Deformation. - 2. Fractures and Joints. - 3. Introduction to Faults. - 4. Normal Faults. - 5. Thrust Faults. - 6. Strike Slip Faults. - 7. Stress. - 8. Mechanics of Fracturing and Faulting: Experiment and Theory. - 9. Mechanics of Natural Fractures and Faults. - Part II. Ductile Deformation. - 10. The Description of Folds. - 11. Foliations and Lineations in Deformed Rocks. - 12. Geometry of Homogeneous Strain. - 13. Kinematic Analysis of Folds. - 14. Analysis of Foliations and Lineations. - 15. Observations of Strain in Deformed Rocks. - Part III. Rheology. - 16. Macroscopic Aspects of Rock Deformation: Rheology and Experiment. - 17. Microscopic Aspects of Ductile Deformation: Mechanisms and Fabrics. - 18. Scale Models and Quantitative Models of Rock Deformation. - Part IV. Regional Associations of Structures. - 19. Development of Structures at Active Plate Margins. - 20. Anatomy and Tectonics of Orogenic Belts.
    Type of Medium: Monograph available for loan
    Pages: XVI, 736 S. , Ill., graph. Darst., Kt. , 29 cm
    Edition: 2. ed., 3. print.
    ISBN: 9780716749516
    Classification:
    Tectonics
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  • 10
    Monograph available for loan
    Monograph available for loan
    Toronto : Mineralogical Association of Canada ; 23.1995 -
    Associated volumes
    Call number: 11/M 14.0093
    In: Short course handbook
    Type of Medium: Monograph available for loan
    Pages: ix, 319 S. : graph. Darst.
    Series Statement: Short course handbook / Mineralogical Association of Canada 14
    Classification:
    Tectonics
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