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Titlebook: Energetics of Geological Processes; Hans Ramberg on his Surendra K. Saxena,Somdev Bhattacharji,Ove Stephan Book 1977 Springer Science+Busi

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書目名稱Energetics of Geological Processes
副標(biāo)題Hans Ramberg on his
編輯Surendra K. Saxena,Somdev Bhattacharji,Ove Stephan
視頻videohttp://file.papertrans.cn/310/309993/309993.mp4
圖書封面Titlebook: Energetics of Geological Processes; Hans Ramberg on his  Surendra K. Saxena,Somdev Bhattacharji,Ove Stephan Book 1977 Springer Science+Busi
描述Hans Ramberg is working in an area of geology where 60 years are a short, often negligible period of time. This is not so in the lives of men. For us it is a time for evaluating past accomplishments and a time for friends to express their appreciation and admiration. Some universities have become famous for this ability to foster eminent scientists in one or several fields. The success of Cambridge University in physics is a well-known example, but if we ask ourselves whether the success of Oslo University in earth sciences is not equally astonishing, then we see that Hans is yet another example of this process; but it is not the whole story. There were certainly promising prospects when he started his studies in geology: V. M. Goldschmidt had just come back from G6ttingen in Germany and Tom Barth had returned from the Geophysical Laboratory in Washington, D.C. Two leaders in geochemistry and petrology at the same time! Hans became a student of Barth, specializing in metamorphic rocks and their problems; but soon the situation changed. Norway was occupied by the Germans and the possibili- ties for university studies almost vanished. However, in spite of all difficulties he obtained
出版日期Book 1977
關(guān)鍵詞Energetics; Geochemie; Geodynamik; Ramberg, Hans; geochemistry; geoscience
版次1
doihttps://doi.org/10.1007/978-3-642-86574-9
isbn_softcover978-3-642-86576-3
isbn_ebook978-3-642-86574-9
copyrightSpringer Science+Business Media New York 1977
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Seiteneinsteiger finden und analysieren,ns of the mineral phases register the activities of the reactive fluid components in a metamorphic terrain. The same relations also permit graphical representation of the stability relations of minerals of fixed compositions as functions of the activities of fluid components at constant . and .. The
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https://doi.org/10.1007/978-3-663-05177-0e critical temperature range between 675°C and 475°C. No absolute values for the cooling rates at Phillipston can, therefore, be extracted from the measured composition profiles. We have used our model and the measured composition profiles, however, to refine our meager knowledge of the temperature
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