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Titlebook: Lectures in Isotope Geology; Emilie Jäger,Johannes C. Hunziker Conference proceedings 1979 Springer-Verlag Berlin Heidelberg 1979 Diffusio

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书目名称Lectures in Isotope Geology
编辑Emilie Jäger,Johannes C. Hunziker
视频videohttp://file.papertrans.cn/584/583450/583450.mp4
图书封面Titlebook: Lectures in Isotope Geology;  Emilie Jäger,Johannes C. Hunziker Conference proceedings 1979 Springer-Verlag Berlin Heidelberg 1979 Diffusio
描述Our colleagues from the French-speaking parts of Switzerland - the Suisses romands - and above all the committee of the 3rd Cycle, e Earth Sciences (3 Cycle, Sciences de la Terre) honored us by asking us to give a course on Isotope Geology for the year 1977. The course, entitled Evaluation et Interpretation des Donnees Isotopiques (eval­ uation and Interpretation of Isotopic Data), was intended to inform earth scientists, graduate and postgraduate, from the western Swiss Universities on the subject of Isotope Geology. Such courses usually consist of two parts: lectures and excursions. Thus, in March 1977, we gave such a two-week course at the Miner­ alogical Institute of the University of Berne. The first week was devoted essentially to the methods of dating, the second week to the behavior of stable isotopes. In July 1977, on the occasion of an excursion to the Central and Western Alps, we were able to demonstrate our results. Guest professors were invited to make contributions to the course.
出版日期Conference proceedings 1979
关键词Diffusion; Geology; Isotop; Isotope; geochemistry; geoscience
版次1
doihttps://doi.org/10.1007/978-3-642-67161-6
isbn_softcover978-3-540-09158-5
isbn_ebook978-3-642-67161-6
copyrightSpringer-Verlag Berlin Heidelberg 1979
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Correction and Interpretation of Fission Track Ages, formation of the sample was not met. It is now known that track retention is a very temperature-sensitive and characteristic property of minerals and natural glasses. The understanding of track retention is the key for the proper interpretation of fission track ages.
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Diffusion Experiments in Isotope Geology,r stops completely (except at absolute zero temperature), and it can therefore equilibrate minerals . when the rock is sufficiently close to . equilibrium so that other reaction mechanism cease to operate.
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Thermal Models of the Central Alps, unrelated quantities can be visualized if one realizes that rock moving towards the surface (as it does when undergoing uplift and denudation) carries the isothermal surfaces upwards. Since the surface of the ground is essentially at a constant temperature, denudation tends to steepen the near-surface. geothermal gradient.
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Conference proceedings 1979 Cycle, Sciences de la Terre) honored us by asking us to give a course on Isotope Geology for the year 1977. The course, entitled Evaluation et Interpretation des Donnees Isotopiques (eval­ uation and Interpretation of Isotopic Data), was intended to inform earth scientists, graduate and postgraduat
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Theory of Cooling Ages,emperatures”, that is, temperatures at which the various systems start to retain their radiogenic daughter products. Above its blocking temperature each system appears to lose its daughter product completely, and below it the daughter product is quantitatively retained.
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