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Titlebook: Regional Stratigraphy of North America; William J. Frazier,David R. Schwimmer Book 1987 Plenum Press, New York 1987 Continental shelf.Delt

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書(shū)目名稱Regional Stratigraphy of North America
編輯William J. Frazier,David R. Schwimmer
視頻videohttp://file.papertrans.cn/826/825377/825377.mp4
圖書(shū)封面Titlebook: Regional Stratigraphy of North America;  William J. Frazier,David R. Schwimmer Book 1987 Plenum Press, New York 1987 Continental shelf.Delt
描述An early reviewer of this book stated that he had difficulty assessing its marketability because it "falls between the cracks" of geological literature. We have designed this book to meet a need of modem geology: namely, a single source providing both detailed and synoptic stratigraphy of the various regions of North America, through geological time. Shortly after beginning work on such a book, we realized why it had not yet been written: it required six years of effort, assimilation of an incredible amount of information, and two years‘ additional work to cut the volume down to publishable size. Further, by the time the final chapter was written, the fIrst few were already out of date. Nevertheless, the book lies in front of you. It is intended to serve several purposes. As a textbook, it will serve the following courses: ? Regional stratigraphy ? Sedimentary tectonics ? Regional tectonics ? Advanced historical geology ? Survey-level paleontology Obviously, not all portions of the book are relevant to all of the above courses. We assume the reader will retain this book after the particular course is done, and will use it as a reference book. Hopefully, others will obtain the book
出版日期Book 1987
關(guān)鍵詞Continental shelf; Deltas; North America; assimilation; formation; geology; historical geology; paleontolog
版次1
doihttps://doi.org/10.1007/978-1-4613-1795-1
isbn_ebook978-1-4613-1795-1
copyrightPlenum Press, New York 1987
The information of publication is updating

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,The Sauk Sequence: Ediacarian—Lower Ordovician, will be based on the cratonic sequences of L. L. Sloss, which reflect natural stratigraphic breaks in response to waxing and waning of the epeiric seas which have characterized much of North America’s Paleozoic and Mesozoic history.
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,The Zuni Sequence: Middle Jurassic—Upper Cretaceous,areas of Zuni sedimentation were: in the western craton and Cordillera, reaching from Alaska to Mexico; on the eastern continental margin, where the Atlantic Coastal Plain first developed during this time; and on the Gulf Coastal Plain, along with the birth of the Gulf of Mexico.
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