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OverviewThe principal aim of the present work is to understand the evolution of halogenesis in the Paleozoic. To succeed in the study it was neces- sary to make a general and systematic synthesis of data available on world-wide Paleozoic halogenic deposits and describe all known eva- porite basins. This study succeeds the monograph Paleozoic Salt For- mations of the World (Zharkov 1974a). The history of Paleozoic salt accumulation is based chiefly on evidence presented in the above monograph; this work should be considered as its direct continutation. The present work mainly aims at: (1) establishment of the num- ber of both salt and sulfate basins and salt and sulfate sequences formed therein in the Paleozoic; (2) determination of the stratigraphic position of salt and sulfate sequences in separate regions, their distant correlation and recognition of stages of evaporite sedimentation during the Paleozoic; (3) determination of the volume and areas of distribution of halite, potash, and sulfate sedimentation within basins and on continents through periods, epochs, and ages of the Paleozoic to single out epochs of the most intense evaporite sedimentation; (4) reconstruction of paleogeography of continents to recognize stages of evaporite accumulation and paleoclimatic zones of halogenic sedi- mentation in the Paleozoic; (5) understanding the evolution of eva- porite sedimentation in the Paleozoic. The nomenclature used in the book should be explained. Full Product DetailsAuthor: M. A. Zharkov , A. L. Yanshin , R. E. Sorkina , R. V. FursenkoPublisher: Springer-Verlag Berlin and Heidelberg GmbH & Co. KG Imprint: Springer-Verlag Berlin and Heidelberg GmbH & Co. K Weight: 0.650kg ISBN: 9783540106142ISBN 10: 3540106146 Pages: 316 Publication Date: 01 May 1981 Audience: Professional and scholarly , Professional & Vocational Format: Hardback Publisher's Status: Active Availability: Out of stock ![]() The supplier is temporarily out of stock of this item. It will be ordered for you on backorder and shipped when it becomes available. Table of ContentsI Distribution and Number of Paleozoic Evaporite Sequences and Basins.- Cambrian Evaporite Deposits.- Ordovician Evaporite Deposits.- Silurian Evaporite Deposits.- Devonian Evaporite Deposits.- Carboniferous Evaporite Deposits.- Permian Evaporite Deposits.- General Conclusions.- II Stratigraphic Position of Evaporites and Stages of Evaporite Accumulation.- Statement of the Problem.- Stratigraphic Position of Cambrian Evaporites.- Stratigraphic Position of Ordovician Evaporites.- Stratigraphic Position of Silurian Evaporites.- Stratigraphic Position of Devonian Evaporites.- Stratigraphic Position of Carboniferous Evaporites.- Stratigraphic Position of Permian Evaporites.- Stages of Sulfate, Halite, and Potassium Accumulation in the Paleozoic.- III Areal Extent and Volume of Evaporites. Epochs of Intense Evaporite Accumulation.- Introductory Remarks.- Areal Extent and Volume of Halogenic Rocks in Paleozoic Evaporite Basins.- Areal Extent of Evaporites During Various Periods, Epochs, and Ages of the Paleozoic.- The Volume of Evaporite Sedimentation in Different Periods, Epochs, and Ages of the Paleozoic.- General Conclusions.- IV Paleogeography of Continents and Paleoclimatic Zonation of Evaporite Sedimentation.- Introductory Remarks.- Paleogeography of Continents and Paleoclimatic Zonation for Evaporite Sedimentation in the Early Cambrian.- Reconstruction Without Regard for Continental Drift.- Reconstruction Which Invokes Continental Drift.- Conclusions Concerning Paleoclimate and Paleogeography of Evaporite Basins in the Early Cambrian.- Paleogeography of Continents and Paleoclimatic Zonation of Evaporite Sedimentation for the Middle and Late Devonian.- Reconstruction Which Does Not Invoke Continental Drift.- Reconstruction Which Invokes Continental Drift.- Conclusions Concerning Paleoclimate and Paleogeography of Evaporite Basins During the Middle and Late Devonian.- Paleogeography of Continents and Paleoclimatic Zonation of Evaporite Sedimentation in the Permian.- Reconstruction Which Does Not Invoke Continental Drift.- Reconstruction Which Invokes Continental Drift.- Conclusions Concerning Paleoclimate and Paleogeography of Evaporite Basins During the Permian.- Main Paleogeographic and Paleoclimatic Features of Paleozoic Evaporite Sedimentation.- EPILOG Evolution of Evaporite Sedimentation in the Paleozoic.- References.ReviewsAuthor InformationTab Content 6Author Website:Countries AvailableAll regions |