| 书目名称 | São Francisco Craton, Eastern Brazil | | 副标题 | Tectonic Genealogy o | | 编辑 | Monica‘Heilbron,Umberto G. Cordani,Fernando F. Alk | | 视频video | | | 概述 | Examines the tectonic genealogy and development history of the Sao Francisco Craton, a ‘miniature continent‘ located in Eastern Brazil.Provides a panorama of the evolutionary history of a piece of con | | 丛书名称 | Regional Geology Reviews | | 图书封面 |  | | 描述 | The region of the São Francisco river valley in eastern Brazil encompasses two main components of the geologic framework of the South American continent: the São Francisco craton and its marginal orogenic belts. Cratons, as the oldest, differentiated and relatively stable pieces of the continental lithosphere, preserve a substantial part of the Earth‘s memory. Orogenic belts, on the other hand, record collisional processes that occurred during a limited time span. Because of their topographic relief, mountain belts developed along craton margins provide however access to rock successions not exposed in the low lands of the adjacent cratons. The combination of geologic information obtained in cratonic domains and their marginal orogenic belts thus form the basis for deciphering substantial periods of Earth’s history. .Corresponding to the most intensively studied portion of the Precambrian nucleus of the South American plate, the São Francisco craton and its margins host a rock record that spans from the Paleoarchean to the Cenozoic. Precambrian sedimentary successions that witness ancient Earth processes - many of them of global significance - are especially well preserved and expo | | 出版日期 | Book 2017 | | 关键词 | Continental Lithosphere; Orogenic Belt; Paleoarchean; Sao Francisco Craton; South American Plate; structu | | 版次 | 1 | | doi | https://doi.org/10.1007/978-3-319-01715-0 | | isbn_softcover | 978-3-319-79130-2 | | isbn_ebook | 978-3-319-01715-0Series ISSN 2364-6438 Series E-ISSN 2364-6446 | | issn_series | 2364-6438 | | copyright | Springer International Publishing Switzerland 2017 |
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发表于 2025-3-21 18:10:31
