| 书目名称 | Gondwana Industrial Clays | | 副标题 | Tandilia System, Arg | | 编辑 | Patricia Eugenia Zalba,Martín Eduardo Morosi,María | | 视频video | | | 概述 | Studies the world’s oldest Gondwana industrial clays.Written by experts in the field of mineralogy and geology in South America.Provides insights into economically important sedimentary and residual d | | 丛书名称 | Springer Earth System Sciences | | 图书封面 |  | | 描述 | .This book is a study of the sedimentary and residual deposits of the Tandilia System, also known as the Sierras Septentrionales of Buenos Aires, Argentina. Offering an overview of the geology, stratigraphy, petrology, mineralogy and industrial applications of these deposits, it is organized geographically and according to the different districts of the province’s diverse counties where economically important Neoproterozoic and Eopaleozoic clay reserves occur..Today, most of the sediments of the Tandilia basin are found in South Africa due to the breakup of the continents, which began in the Jurassic. This partly accounts for the difficulty in interpreting the geology of Tandilia. Apart from its extreme age and almost complete lack of fossil remains, for a long time the tectonics that affected the whole area presented a real challenge, as horst and graben structures added to the difficulty of geological correlations. Despite being 700 Ma old, most of the physical-chemical properties of the sediments have remained unchanged. The Microbially Induced Sedimentary Structures (MISS) found in the tidal and peritidal deposits also hold untouched information on the mystery of the beginning | | 出版日期 | Book 2016 | | 关键词 | Gondwana Industrial Clays; Argentina; Tandilia System; Neoproterozoic Clays; Eopaleozoic Clays; Geology; M | | 版次 | 1 | | doi | https://doi.org/10.1007/978-3-319-39457-2 | | isbn_softcover | 978-3-319-81890-0 | | isbn_ebook | 978-3-319-39457-2Series ISSN 2197-9596 Series E-ISSN 2197-960X | | issn_series | 2197-9596 | | copyright | Springer International Publishing Switzerland 2016 |
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发表于 2025-3-21 17:24:38
