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Titlebook: Sedimentary Basins; Evolution, Facies, a Gerhard Einsele Textbook 2000Latest edition Springer-Verlag Berlin Heidelberg 2000 Basin dynamics.

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发表于 2025-3-21 16:26:15 | 显示全部楼层 |阅读模式
书目名称Sedimentary Basins
副标题Evolution, Facies, a
编辑Gerhard Einsele
视频video
概述Quantitative approach of basin dynamics.Contains a lot of figures.Most figures are specifically designed for the book.Contains aspects that are not dealt with in other books (e.g. diagenesis, sediment
图书封面Titlebook: Sedimentary Basins; Evolution, Facies, a Gerhard Einsele Textbook 2000Latest edition Springer-Verlag Berlin Heidelberg 2000 Basin dynamics.
描述The modem geological sciences are characterized by extraordinarily rapid prog­ ress, as well as by the development and application of numerous new and refined methods, most of them handling an enormous amount of data available from all the continents and oceans. Given this state of affairs, it searns inevitable that rnany students and profes­ sionals tend to become experts in relatively narrow fields and thereby are in danger of losing a broad view of current knowledge. The abundance of new books and symposium volumes testifies to this trend toward specialization. However, many geologie processes are complex and result from the interaction of many, seemingly unrelated, individual factors. This signifies that we still need generalists who have the broad overview and are able to evaluate the great variety of factors and pro­ ces ses controlling a geologie system, such as a sedimentary basin. In addition, this also means that cooperation with other disciplines in the natural sciences andengi­ neering is increasingly important. Modem text books providing this broad overview of the earth sciences are rare.
出版日期Textbook 2000Latest edition
关键词Basin dynamics; Beckendynamik; Coast; Diagenese; Kompaktion; Ocean; Sediment; Sedimentation; Sequenzstratiga
版次2
doihttps://doi.org/10.1007/978-3-662-04029-4
isbn_softcover978-3-642-08544-4
isbn_ebook978-3-662-04029-4
copyrightSpringer-Verlag Berlin Heidelberg 2000
The information of publication is updating

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发表于 2025-3-21 22:46:05 | 显示全部楼层
Continental Sedimentst variety of features characteristic of glacial environments, including many minor structures and patterns which can be observed at or near the land surface. Therefore it is barely possible to summarize all these phenomena in a few simple facies models.
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Special Depositional Environments and Sedimentss, but in these cases the minerals causing the green color may differ from those found in young sediments due to diagenesis. The correct identification, crystallographic and geochemical characterization of finegrained green minerals is difficult and can be done only in the laboratory using special m
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Denudation: Solute Transport and Flux Rates of Terrigenous Sedimentr biogenic and chemical sediments, insofar as their production depends on the dissolved river load delivered into the sedimentary basins. The land-derived, solid material is usually referred to as the terrigenous, allochthonous, clastic component of a sedimentary deposit.
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Basin Evolution and Sedimentsphysicists, structural geologists, stratigraphers, and sedimentary geologists is needed. In addition, petroleum geologists contribute considerably to our knowledge about basin evolution. Having in mind the fact that some hundred to thousand sedimentary basins, young and ancient, exist all over the w
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Mechanical and Chemical Diagenesisigh water content. However, with increasing burial depth under younger sediments, and occasionally shortly after deposition, the sediments become denser and more solid or lithified. All the processes involved in such a change of sediment state are summarized under the term .. It comprises both mecha
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