ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Call number: SR 90.0001(1088)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 65 S.
    Series Statement: U.S. Geological Survey bulletin 1088
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Call number: 11/G 9161
    In: Reviews in mineralogy
    Description / Table of Contents: This book has been written mainly to help the newcomer in fluid-inclusion work learn how to use fluid inclusions and to avoid many of the pitfalls and blind alleys that beset anyone starting in a new field of research. Of course, it is impossible to avoid all such diversions. However, too often, writers of scientific papers (and some editors) seem to believe that it is undesirable or even demeaning to report experimental details and the various problems that had to be overcome in the work. I do not agree with this approach. Why should subsequent workers be frustrated and waste much time solving problems that others have already solved? Give them the benefit of previous experience so that they can get on with new work; in so doing, they will encounter enough new problems of their own. One difficulty in presenting a subject such as fluid inclusions is the surprising degree to which the chapters are interrelated. I have tried to strike an appropriate compromise between repeated referral to other chapters and excessive repetition, because everything cannot be put into logical sequence without redundancy. Chapters 11-18 attempt to discuss the many applications of fluid inclusions to the study of and understanding of geologic processes and the geologic environments in which they acted. For the reader's convenience, I have categorized all environments from which fluid inclusions have been studied into these eight chapters. The arbitrary dividing lines between such environments are never sharp, nor generally acceptable, particularly if more than one geologist is asked, so I hope the reader will forgive me if my semantics disagree with his or hers; the differences are of no real consequence to the points being made. Although some of the data and ideas in this book are new, other parts come from earlier papers of my own or from those on which I have been a coauthor. I make no apology for this, as I see no point in using quotation marks or trying to rephrase one's own words. Only about a third of the text is taken more-or-less directly from these earlier works (with modifications). Similarly, many but not all the photomicrographs have been used earlier. In the choice of examples, I have leaned heavily on those from my own experience and papers, mainly because this procedure is less prone to errors from misquotation, and because I have all the negatives of the photomicrographs I made in these studies. In a petrography class, in 1939, my teacher, Dr. Donald M. Fraser, showed me some inclusions in Precambrian quartzite in which the bubbles were rapidly bouncing around in their tiny cells, as they presumably had been for more than a billion years. This so intrigued me that after completing graduate work (more than 30 years ago) I started studying fluid inclusions. I hope that some aspect of this book may, in the same way, intrigue others. I have tried to help the reader by including chapter outlines and a detailed index, and in the References I have listed the page(s) where each item is cited, as this also can help the reader to become acquainted with the rather large and scattered literature and some of its applications. The overall organization is somewhat of an adaptation of the news reporter's outline -- "who. what, when, where, and why": what kinds of information inclusions provide. when and where inclusions form. how they change, how to prepare material and make microthermometric measurementsl, how to interpret these data, and then what has been found in applications of fluid-inclusion studies to each of a series of different geologic environments. As in most developing areas of science, numerous erroneous concepts, procedures, and statements have been published (including some of my own). I have a file of several hundred of these errors, but most do not merit attention and hence are not mentioned in this volume, except where they may have led to more than occasional confusion or misunderstanding by later workers. Caveat emptor.
    Type of Medium: Monograph available for loan
    Pages: vi, 646 S.
    ISBN: 0-939950-16-2 , 978-0-939950-16-4
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 12
    Language: English
    Note: Chapter 1. Introduction to Fluid Inclusions p. 1 - 10 Chapter 2. The Origin of Inclusions p. 11 - 46 Chapter 3. Changes in Inclusions after Trapping p. 47 - 78 Chapter 4. Nondestructive Methods of Determination of Inclusion Composition p. 79 - 108 Chapter 5. Destructive Methods of Determination of Inclusion Composition p. 109 - 148 Chapter 6. Inclusion Sample Selection, Preparation, Petrography, and Photography p. 149 - 180 Chapter 7. Inclusion Measurements -- Heating, Cooling Decrepitation and Crushing p. 181 - 220 Chapter 8. Interpretation and Utilization of Inclusion Measurements -- Compositional Data on Liquid and Gas Inclusions p. 221 - 250 Chapter 9. Interpretation and Utilization of Inclusion Measurements -- Temperature, Pressure and Density at Trapping p. 251 - 290 Chapter 10. Interpretation and Utilization of Inclusion Measurements -- Metastability p. 291 - 304 Chapter 11. Sedimentary Environments p. 305 - 336 Chapter 12. Low- to Medium-Grade Metamorphic Environments p. 337 - 360 Chapter 13. Medium- to High-Grade Metamorphic Environments p. 361 - 380 Chapter 14. Intrusive Rock and Pegmatitic Environments p. 381 - 412 Chapter 15. Ore Deposition Environments p. 413 - 472 Chapter 16. Extrusive Rock and Volcanic Environments p. 473 - 502 Chapter 17. Upper Mantle Environments p. 503 - 532 Chapter 18. Extraterrestrial Environments p. 533 - 570 Chapter 19. Future of Inclusion Studies p. 571 - 584
    Location: Reading room
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Call number: SR 90.0002(440-JJ)
    In: Data of geochemistry
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: X, 164 S.
    Series Statement: 440-JJ
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 411 (2001), S. 155-155 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Discovery of bacteria that remain viable in a dormant state for lengthy periods is significant for understanding patterns of microbial diversity and evolution on Earth, as well as for assessing the possibility of life's interplanetary transport by impact processes. The isolation by Vreeland et ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 293 (1981), S. 459-462 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] I have examined the following sections of the original rock in question (no. 2377): 2377-1-D from J. W. Schopf, UCLA; and 2377,2377-G! and 2377-G2, and a small piece of the rock itself, from H. D. Pflug. The objects vary only in abundance among the four sections. A brief description of the ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 244 (1973), S. 210-212 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Where free of crystals, the orange glass is remarkably uniform in composition from one particle to another (Table 1). The composition is that of an ilmenite-olivine mare basalt, as shown by the CIPW norm. About 0.2% of spherules 〉150 mm contain coarse, solid, sharply euhedral, unzoned Fo88 ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 267 (1977), S. 558-559 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] VISSER and Koster van Groos1 present a new phase equilibrium diagram for the plane leucite^fayalite-SiO2 in the quaternary system KaO-FeO-Al2O3-SiO2, in which the field of immiscibility differs significantly from that which I presented earlier2, and from that presented by Greig on the binary ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 315 (1985), S. 544-545 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] FLUID inclusions are small droplets of the fluids from which crystals grew and are found in many minerals, both natural and synthetic. In natural gem minerals, fluid inclusions diminish their clarity, and hence their value; in synthetic crystals they detract from the useful mechanical, electrical ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 56 (1994), S. 23-28 
    ISSN: 1432-0819
    Keywords: carbon dioxide ; fluid inclusions ; plagioclase ; tholeiite magma ; Moeraki (NZ)
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Liquid plus vapour inclusions of CO2 are widespread in plagioclase microphenocrysts in small tholeiitic intrusions and tephra of the Moeraki and adjacent areas of northeast Otago, New Zealand. They imply the presence of immiscible CO2 droplets in the magma at depths of about 7–14 km. Their presence within 5 μm of the edges of microphenocrysts as little as 35 μm thick and 118 μm long indicates minimal feldspar crystal growth during the final ascent and quenching of the magma. Delicate branching clusters of lath-like microphenocrysts escaped disruption during this ascent. Such CO2 inclusions are a potential source of ‘excess argon’ perturbing K−Ar age determinations.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 56 (1994), S. 23-28 
    ISSN: 1432-0819
    Keywords: Key words: carbon dioxide – fluid inclusions – plagioclase – tholeiite magma – Moeraki (NZ)
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract. Liquid plus vapour inclusions of CO2 are widespread in plagioclase microphenocrysts in small tholeiitic intrusions and tephra of the Moeraki and adjacent areas of northeast Otago, New Zealand. They imply the presence of immiscible CO2 droplets in the magma at depths of about 7–14 km. Their presence within 5 μm of the edges of microphenocrysts as little as 35 μm thick and 118 μm long indicates minimal feldspar crystal growth during the final ascent and quenching of the magma. Delicate branching clusters of lath-like microphenocrysts escaped disruption during this ascent. Such CO2 inclusions are a potential source of ‘excess argon’ perturbing K-Ar age determinations.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...