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Titlebook: Geological Evolution of the Earth During the Precambrian; Lazarus J. Salop Book 1983 Springer-Verlag Berlin Heidelberg 1983 Cambrian.Geolo

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發(fā)表于 2025-3-21 17:13:07 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱(chēng)Geological Evolution of the Earth During the Precambrian
編輯Lazarus J. Salop
視頻videohttp://file.papertrans.cn/384/383316/383316.mp4
圖書(shū)封面Titlebook: Geological Evolution of the Earth During the Precambrian;  Lazarus J. Salop Book 1983 Springer-Verlag Berlin Heidelberg 1983 Cambrian.Geolo
描述Progress in Precambrian geology has been exceptionally great, indeed quite striking for geologists of the older generation; only some 30-40 years ago the Precambrian appeared as an uncertain and even mystic prelude to geologic evolution. Even the very name - Precambrian - means some indi- visible unit in the early history of the Earth, the beginning of which is poorly known. At the same time it was obvious that the Precambrian formations are of extremely varied and complex composition and poor knowledge and lack of reliable methods of division and correlation were to blame for the lack of significant progress in studies of this early evolutionary stage of the planet. Certainly, even at the very start of Precambrian studies, the results obtained were quite promising, lifting as they did the mysterious veil over the regional Precambrian; but they presented no general realistic picture of this early stage in the Earth‘s evolution at that time. Recently, this situation has completely changed, due to new methods of study of the older forma- tions, and due also to the refinement of some well-known methods, in particular of division, dating, and correlation of "silent" metamorphic strata.
出版日期Book 1983
關(guān)鍵詞Cambrian; Geologie; Pr?kambrium; atmosphere; environment; evolution; formation; geology; history; isotope; sed
版次1
doihttps://doi.org/10.1007/978-3-642-68684-9
isbn_softcover978-3-642-68686-3
isbn_ebook978-3-642-68684-9
copyrightSpringer-Verlag Berlin Heidelberg 1983
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發(fā)表于 2025-3-22 00:00:41 | 只看該作者
https://doi.org/10.1007/978-3-642-68684-9Cambrian; Geologie; Pr?kambrium; atmosphere; environment; evolution; formation; geology; history; isotope; sed
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Geologic Synthesis,ities of geologic evolution of each of these units were pointed out. Some general problems of geologic (mainly tectonic) evolution ensuing from the analysis will be briefly outlined in this chapter. In the first place these are the cyclicity, tendency, and continuity (inheritance) of geologic processes.
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Geological Evolution of the Earth During the Precambrian978-3-642-68684-9
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Book 1983his early stage in the Earth‘s evolution at that time. Recently, this situation has completely changed, due to new methods of study of the older forma- tions, and due also to the refinement of some well-known methods, in particular of division, dating, and correlation of "silent" metamorphic strata.
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The Theoretical Analysis of Political Risk,below. The basement of the erathem is unknown. In many regions of the world the supracrustals and plutonic rocks are unconformably overlain by the Paleoprotozoic (Archeoprotozoic) greenstone strata, but their original relations are commonly masked by later thermal-tectonic processes.
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