# ALBERT

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• 1
Monograph available for loan
Princeton, N.J. : Princeton Univ. Press
Call number: M 15.0249
Type of Medium: Monograph available for loan
Pages: 386 S. : graph. Darst.
Location: Upper compact magazine
Branch Library: GFZ Library
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• 2
Monograph available for loan
Washington, D.C. : Mineralogical Society of America
Associated volumes
Call number: 11/M 96.0480
In: Reviews in mineralogy
Type of Medium: Monograph available for loan
Pages: xx, 862 S.
ISBN: 0-939950-41-3 , 978-0-939950-41-6
ISSN: 1529-6466
Series Statement: Reviews in mineralogy 33
Classification: A.3.6.
Language: English
Note: Chapter 1. Mineralogy, Petrology and Geochemistry of Boron: An Introduction by Lawrence M. Anovitz and Edward S. Grew, p. 1 - 40 Chapter 2. The Crystal Chemistry of Boron by Frank C. Hawthorne, Peter C. Burns, and Joel D. Grice, p. 41 - 116 Chapter 3. Experimental Studies on Borosilicates and Selected Borates by G. Werding and Werner Schreyer, p. 117 - 164 Chapter 4. Thermochemistry of Borosilicate Melts and Glasses - from Pyrex to Pegmatites by Alexandra Navrotsky, p. 165 - 180 Chapter 5. Thermodynamics of Boron Minerals: Summary of Structural, Volumetric and Thermochemical Data by Lawrence M. Anovitz and Bruce S. Hemingway, p. 181 - 262 Chapter 6. Continental Borate Deposits of Cenozoic Age by George I. Smith and Marjorie D. Medrano, p. 263 - 298 Chapter 7. Boron in Granitic Rocks and Their Contact Aureoles by David London, George B. Morgan, VI, and Michael B. Wolf, p. 299 - 330 Chapter 8. Experimental Studies of Boron in Granitic Melts by Donald B. Dingwell, Michel Pichavant, and François Holtz, p. 331 - 386 Chapter 9. Borosilicates (Exclusive of Tourmaline) and Boron in Rock-forming Minerals in Metamorphic Environments by Edward S. Grew, p. 387 - 502 Chapter 10. Metamorphic Tourmaline and Its Petrologic Applications by Darrell J. Henry and Barbara L. Dutrow, p. 503 - 558 Chapter 11. Tourmaline Associations with Hydrothermal Ore Deposits by John F. Slack, p. 559 - 644 Chapter 12. Geochemistry of Boron and Its Implications for Crustal and Mantle Processes by William P. Leeman and Virginia B. Sisson, p. 645 - 708 Chapter 13. Boron Isotope Geochemistry: An Overview by Martin R. Palmer and George H. Swihart, p. 709 - 744 Chapter 14. Similarities and Contrasts in Lunar and Terrestrial Boron Geochemistry by Denis M. Shaw, p. 745 - 770 Chapter 15. Electron Probe Microanalysis of Geologic Materials for Boron by James J. McGee and Lawrence M. Anovitz, p. 771 - 788 Chapter 16. Analyses of Geological Materials for Boron by Secondary Ion Mass Spectrometry by Richard L. Hervig, p. 789 - 804 Chapter 17. Nuclear Methods for Analysis of Boron in Minerals by J. David Robertson and M. Darby Dyar, p. 805 - 820 Chapter 18. Parallel Electron Energy-loss Spectroscopy of Boron in Minerals by Laurence A. J. Garvie and Peter R. Buseck, p. 821 - 844 Chapter 19. Instrumental Techniques for Boron Isotope Analysis by George H. Swihart, p. 845 - 862
Branch Library: GFZ Library
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• 3
Series available for loan
Canberra : Australian Gov. Publ. Service
Associated volumes
Call number: SR 93.0764(272)
In: Report
Type of Medium: Series available for loan
Pages: IV, 26 S.
ISBN: 0644048824
Series Statement: Report / Department of Resources & Energy, Bureau of Mineral Resources, Geology & Geophysics 272
Language: English
Location: Lower compact magazine
Branch Library: GFZ Library
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• 4
Unknown
Chantilly, Va. : Mineralogical Society of America
Pages: Online-Ressource (xiv, 491 Seiten)
ISBN: 9780939950966
Language: English
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• 5
Electronic Resource
Springer
ISSN: 1432-0967
Source: Springer Online Journal Archives 1860-2000
Topics: Geosciences
Type of Medium: Electronic Resource
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• 6
Electronic Resource
Springer
ISSN: 1432-0967
Source: Springer Online Journal Archives 1860-2000
Topics: Geosciences
Notes: Abstract The template transformation allows rapid straight line plotting of fluid-bearing reactions for conditions exceeding the two phase field in water-carbon dioxide. The system CaO-MgO-SiO2-H2O-CO2 with the six solid phase tale, tremolite, quartz, magnesite, calcite, and dolomite is treated at 2Kb. These phases, in T-NH2O space at constant pressure, participate in two invariant points and eight reactions. Published T-NH2O data for three of these reactions at 2Kb are transformed using the template into LnK-1/T space to yield the parameters of the best (by eye) straight lines. The parameters of the other five reaction lines are derived by linear combination of these parameters. The reactions belonging to one invariant point in T-NH2O space will be straight lines that intersect at a single point in ln K-1/T space. This point is not the transformation of the invariant point, and it occurs because of the linear relationship between the reactions. Errors need to be considered in transforming the system back into T-NH2O space, especially when reactions lines with shallow slopes are involved.
Type of Medium: Electronic Resource
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• 7
Electronic Resource
Springer
ISSN: 1432-0967
Source: Springer Online Journal Archives 1860-2000
Topics: Geosciences
Notes: Abstract A retrograde assemblage in a specimen from the Franklin Marble Formation containing an unusual occurrence of three micas has been studied. Microprobe analyses of the margarite, muscovite and phlogopite reveal significant sodium and fluorine but otherwise show little mutual solid solution. The conditions that prevailed during the retrogression estimated from phase equilibria are T=370–450° C and $$X_{{\text{CO}}_{\text{2}} }$$ =0.03–0.3 at an assumed pressure of 2 kb. Examination of the phlogopite by TEM revealed replacement of phlogopite by chlorite. The chlorite occurred as small packets of layers interlayered with phlogopite. AEM analyses revealed that the chlorite composition approximates that of clinochlore. Transformations from a single phlogopite layer to one chlorite layer (a 1∶1 reaction) and also from two phlogopite layers to one chlorite layer (a 2∶1 reaction) have been observed. Both reactions result in a large volume change causing local strain at transition fronts. An apparently strain-free, volume-preserving transformation of 14 phlogopite layers terminating against 10 chlorite layers was observed which indicates that pervasive replacement may occur through a combination of both reactions. Topological and site occupancy changes during the transformation suggest that the reaction involves not only gain and loss of layer units, but also considerable local rupturing and reformation of bonds, concomitant with ion diffusion and interchange. Dislocations (layer terminations) at the transition front imply the existence of pathways for the fluid flow and ion transport required for mass balance.
Type of Medium: Electronic Resource
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• 8
Electronic Resource
Springer
ISSN: 1432-0967
Source: Springer Online Journal Archives 1860-2000
Topics: Geosciences
Notes: Abstract A computerised algorithm is used to arrange fluid-absent reactions about invariant points in P—T space for an end-member model of blueschist facies metamorphism at Port Macquarie, N.S.W., consisting of the nine phases quartz, albite, jadeite, lawsonite, zoisite, paragonite, glaucophane, pyrope and chlorite. Inspection of the print-out (a table of reaction take-off angles for each invariant point) indicates that this multisystem consists of two mutually exclusive sets of invariant points; lawsonite-absent, paragonite-absent and glaucophane-absent versus the other six. The algorithm is completely general for any two intensive variables and can treat solid solution minerals or degeneracy in reactions/invariant points.
Type of Medium: Electronic Resource
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• 9
Electronic Resource
Springer
Theoretical and applied genetics 73 (1987), S. 856-862
ISSN: 1432-2242
Keywords: Ribulose 1,5 ; Bisphosphate carboxylase oxygenase ; Small subunit ; Nuclear control of Rubisco ; Medicago
Source: Springer Online Journal Archives 1860-2000
Topics: Biology
Notes: Summary The response to selection for leaf proteins was studied during three selection cycles. Selection for high total nitrogen content showed 75% heritability, and the levels of both ribulose 1,5-bisphosphate carboxylase oxygenase (Rubisco) and cytoplasmic protein were strongly under nuclear DNA control. High and low protein content were correlated with chloroplast area. Although the amounts of nuclear DNA were similar, the ratio of Rubisco/DNA and chlorophyll/DNA changed during the selection process. It can be concluded that the levels of Rubisco achieved in mature plants of M. sativa are under nuclear DNA control. The possible involvement of small subunit (SSU) genes in controlling these levels is discussed.
Type of Medium: Electronic Resource
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• 10
Electronic Resource
Springer
Economic theory 3 (1993), S. 99-107
ISSN: 1432-0479
Source: Springer Online Journal Archives 1860-2000
Topics: Economics
Notes: Summary This paper generalizes the Theorem of the Maximum (Berge [2]) to allow for discontinuous changes in the domain and the objective function. It also provides a geometrical version of the (generalized) theorem.
Type of Medium: Electronic Resource
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