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Titlebook: Carbonate Facies in Geologic History; James L. Wilson Textbook 1975 Springer-Verlag Berlin · Heidelberg 1975 Fazies.Gestein.Jura.Karbonatg

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書(shū)目名稱(chēng)Carbonate Facies in Geologic History
編輯James L. Wilson
視頻videohttp://file.papertrans.cn/222/221674/221674.mp4
叢書(shū)名稱(chēng)Springer Study Edition
圖書(shū)封面Titlebook: Carbonate Facies in Geologic History;  James L. Wilson Textbook 1975 Springer-Verlag Berlin · Heidelberg 1975 Fazies.Gestein.Jura.Karbonatg
描述Since 1950 geologists have learned more about the origin and lithification of carbonate sediments than in all the previous years of the history of science. This is true in all the diverse fields of carbonate geology: the study of Recent environments, marine zoology and botany, organic geochemistry, trace element and isotope geochemistry, mineralogy, microfacies of depositional environments, and trace-fossil and sedimentary structure investigation. A synthesis of this new knowledge is just beginning to be formulated. The purpose of this volume is to introduce the advanced student and petroleum explorationist principally to one important aspect of this study: to some of the principles of carbonate geology which may serve to interpret the depositional environments of ancient strata and to better define their sequences and patterns. Chapter I is a brief review of principles of carbonate sedimentation. (For a full discussion of the mineralogy, geochemistry, and diagenesis of carbonates along with a review of Holocene sediments, one may refer to Bathurst‘s (1971) and Milliman‘s (1974) texts.) Chapter II reviews stratigraphic and paleotectonic concepts and discusses a general model for ca
出版日期Textbook 1975
關(guān)鍵詞Fazies; Gestein; Jura; Karbonatgestein; Trias; diagenesis; environment; geochemistry; geology; mineral; minera
版次1
doihttps://doi.org/10.1007/978-1-4612-6383-8
isbn_softcover978-0-387-90343-9
isbn_ebook978-1-4612-6383-8Series ISSN 0172-6234
issn_series 0172-6234
copyrightSpringer-Verlag Berlin · Heidelberg 1975
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Late Paleozoic Terrigenous-Carbonate Shelf Cycles,e persistence of platforms situated just at sea level, the tectonic activity which provided periodic incursions of terrigenous clastics, and the enhanced possibilities of eustatic sea-level fluctuations (either glacially or tectonically induced) all coincided to make this time in earth history favorable for cyclic sedimentation.
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Luca Patanè,Roland Strauss,Paolo Arena offer numerous examples of facies patterns in a variety of tectonic settings, all of which serve to test some of the stratigraphie ideas set forth below. A summary Chapter repeats most of these generalizations.
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Networks Equations and Analysis Methodsareas, the Waulsortian mounds and lenses appear chiefly as an intermediate (shelf margin) facies between geosynclinal basins and shelf deposits which were formed in conditions of open marine circulation (Fig. V-1).
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https://doi.org/10.1007/978-3-030-16194-1mework both within shelf mounds and along shelf margins. They are significant constituents of reservoir rock in some of the world’s greatest oil fields. In this Chapter a discussion of rudist morphology and paleoecology is followed by a description of some typical Middle Cretaceous facies patterns.
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