| 書目名稱 | Fluids in the Crust | | 副標(biāo)題 | Equilibrium and tran | | 編輯 | K. I. Shmulovich,B. W. D. Yardley,G. G. Gonchar | | 視頻video | http://file.papertrans.cn/345/344693/344693.mp4 | | 圖書封面 |  | | 描述 | 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 ad | | 出版日期 | Book 1995 | | 關(guān)鍵詞 | Greisen; carr; formation; metamorphism; mineral; mineralogy; temperature; thermodynamics; transport; water; ec | | 版次 | 1 | | doi | https://doi.org/10.1007/978-94-011-1226-0 | | isbn_softcover | 978-94-010-4536-0 | | isbn_ebook | 978-94-011-1226-0 | | copyright | Chapman & Hall 1995 |
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