Fluids in the Crust: Equilibrium and transport properties
For much of the 20th century, scientific contacts between the Soviet Union and western countries were few and far between, and often super ficial. In earth sciences, ideas and data were slow to cross the Iron Curtain, and there was considerable mutual mistrust of diverging scient ific philosophies....
Gespeichert in:
Weitere Verfasser: | , , |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Dordrecht
Springer Netherlands
1995
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Schlagworte: | |
Online-Zugang: | BTU01 URL des Erstveröffentlichers |
Zusammenfassung: | For much of the 20th century, scientific contacts between the Soviet Union and western countries were few and far between, and often super ficial. In earth sciences, ideas and data were slow to cross the Iron Curtain, and there was considerable mutual mistrust of diverging scient ific philosophies. In geochemistry, most western scientists were slow to appreciate the advances being made in the Soviet Union by os. Korz hinskii, who put the study of ore genesis on a rigorous thermodynamic basis as early as the 1930s. Korzhinskii appreciated that the most fun damental requirement for the application of quantitative models is data on mineral and fluid behaviour at the elevated pressures and temper atures that occur in the Earth's crust. He began the work at the Institute of Experimental Mineralogy (IEM) in 1965, and it became a separate establishment of the Academy of Sciences in Chernogolovka in 1969. The aim was to initiate a major programme of high P-T experimental studies to apply physical chemistry and thermodynamics to resolving geological problems. For many years, Chernogolovka was a closed city, and western scient ists were unable to visit the laboratories, but with the advent of peres troika in 1989, the first groups of visitors were eagerly welcomed to the IEM. What they found was an experimental facility on a massive scale, with 300 staff, including 80 researchers and most of the rest pro viding technical support |
Beschreibung: | 1 Online-Ressource (XIV, 323 p) |
ISBN: | 9789401112260 |
DOI: | 10.1007/978-94-011-1226-0 |
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520 | |a For much of the 20th century, scientific contacts between the Soviet Union and western countries were few and far between, and often super ficial. In earth sciences, ideas and data were slow to cross the Iron Curtain, and there was considerable mutual mistrust of diverging scient ific philosophies. In geochemistry, most western scientists were slow to appreciate the advances being made in the Soviet Union by os. Korz hinskii, who put the study of ore genesis on a rigorous thermodynamic basis as early as the 1930s. Korzhinskii appreciated that the most fun damental requirement for the application of quantitative models is data on mineral and fluid behaviour at the elevated pressures and temper atures that occur in the Earth's crust. He began the work at the Institute of Experimental Mineralogy (IEM) in 1965, and it became a separate establishment of the Academy of Sciences in Chernogolovka in 1969. The aim was to initiate a major programme of high P-T experimental studies to apply physical chemistry and thermodynamics to resolving geological problems. For many years, Chernogolovka was a closed city, and western scient ists were unable to visit the laboratories, but with the advent of peres troika in 1989, the first groups of visitors were eagerly welcomed to the IEM. What they found was an experimental facility on a massive scale, with 300 staff, including 80 researchers and most of the rest pro viding technical support | ||
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illustrated | Not Illustrated |
indexdate | 2024-07-10T08:10:48Z |
institution | BVB |
isbn | 9789401112260 |
language | English |
oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567380 |
oclc_num | 1053844391 |
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physical | 1 Online-Ressource (XIV, 323 p) |
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publishDate | 1995 |
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publisher | Springer Netherlands |
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spelling | Fluids in the Crust Equilibrium and transport properties edited by K. I. Shmulovich, B. W. D. Yardley, G. G. Gonchar Dordrecht Springer Netherlands 1995 1 Online-Ressource (XIV, 323 p) txt rdacontent c rdamedia cr rdacarrier For much of the 20th century, scientific contacts between the Soviet Union and western countries were few and far between, and often super ficial. In earth sciences, ideas and data were slow to cross the Iron Curtain, and there was considerable mutual mistrust of diverging scient ific philosophies. In geochemistry, most western scientists were slow to appreciate the advances being made in the Soviet Union by os. Korz hinskii, who put the study of ore genesis on a rigorous thermodynamic basis as early as the 1930s. Korzhinskii appreciated that the most fun damental requirement for the application of quantitative models is data on mineral and fluid behaviour at the elevated pressures and temper atures that occur in the Earth's crust. He began the work at the Institute of Experimental Mineralogy (IEM) in 1965, and it became a separate establishment of the Academy of Sciences in Chernogolovka in 1969. The aim was to initiate a major programme of high P-T experimental studies to apply physical chemistry and thermodynamics to resolving geological problems. For many years, Chernogolovka was a closed city, and western scient ists were unable to visit the laboratories, but with the advent of peres troika in 1989, the first groups of visitors were eagerly welcomed to the IEM. What they found was an experimental facility on a massive scale, with 300 staff, including 80 researchers and most of the rest pro viding technical support Earth Sciences Mineralogy Economic Geology Earth sciences Economic geology Fluid (DE-588)4017690-3 gnd rswk-swf Erdkruste (DE-588)4015169-4 gnd rswk-swf Erdkruste (DE-588)4015169-4 s Fluid (DE-588)4017690-3 s 1\p DE-604 Shmulovich, K. I. edt Yardley, B. W. D. edt Gonchar, G. G. edt Erscheint auch als Druck-Ausgabe 9789401045360 https://doi.org/10.1007/978-94-011-1226-0 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
spellingShingle | Fluids in the Crust Equilibrium and transport properties Earth Sciences Mineralogy Economic Geology Earth sciences Economic geology Fluid (DE-588)4017690-3 gnd Erdkruste (DE-588)4015169-4 gnd |
subject_GND | (DE-588)4017690-3 (DE-588)4015169-4 |
title | Fluids in the Crust Equilibrium and transport properties |
title_auth | Fluids in the Crust Equilibrium and transport properties |
title_exact_search | Fluids in the Crust Equilibrium and transport properties |
title_full | Fluids in the Crust Equilibrium and transport properties edited by K. I. Shmulovich, B. W. D. Yardley, G. G. Gonchar |
title_fullStr | Fluids in the Crust Equilibrium and transport properties edited by K. I. Shmulovich, B. W. D. Yardley, G. G. Gonchar |
title_full_unstemmed | Fluids in the Crust Equilibrium and transport properties edited by K. I. Shmulovich, B. W. D. Yardley, G. G. Gonchar |
title_short | Fluids in the Crust |
title_sort | fluids in the crust equilibrium and transport properties |
title_sub | Equilibrium and transport properties |
topic | Earth Sciences Mineralogy Economic Geology Earth sciences Economic geology Fluid (DE-588)4017690-3 gnd Erdkruste (DE-588)4015169-4 gnd |
topic_facet | Earth Sciences Mineralogy Economic Geology Earth sciences Economic geology Fluid Erdkruste |
url | https://doi.org/10.1007/978-94-011-1226-0 |
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