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Titlebook: Geology of Southwest Gondwana; Siegfried Siegesmund,Miguel A. S. Basei,Sebastian Book 2018 Springer International Publishing AG, part of

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發(fā)表于 2025-3-21 18:58:55 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Geology of Southwest Gondwana
編輯Siegfried Siegesmund,Miguel A. S. Basei,Sebastian
視頻videohttp://file.papertrans.cn/384/383394/383394.mp4
概述Presents state-of-the-art insights into the geological evolution of Southwest (SW) Gondwana.Offers a review of the accretion of South America and Southern Africa.Includes an updated contribution on th
叢書(shū)名稱Regional Geology Reviews
圖書(shū)封面Titlebook: Geology of Southwest Gondwana;  Siegfried Siegesmund,Miguel A. S. Basei,Sebastian  Book 2018 Springer International Publishing AG, part of
描述. . .This book focuses on the geological evolution of Southwest (SW) Gondwana and presents state-of-the-art insights into its evolution. It addresses the diachronic assembly of continental fragments derived from the break-up of the Rodinia supercontinent later amalgamated to build SW Gondwana during the Neoproterozoic–Cambrian transition, which on a global scale includes parts of present-day South America, Africa and Madagascar. The book presents 24 state-of-the-art reviews including the most crucial controversies. Most experienced scientists about the geology of SW Gondwana from Europe, Africa, South America and Australia present contributions on key areas addressing the interactions between the main cratons and fold belts on both sides of the South Atlantic Ocean. Chapters related to the geology of the major. Archean- Paleoproterozoic cratons and Neoproterozoic Brasiliano/Pan-African fold belts enable readers to gain an in-depth understanding of the tectonometamorphic and magmatic evolution of SW Gondwana. The book covers a wide range of issues including metallogenetic, sedimentary, paleobiological and paleoclimatic processes and allows a deep?insight?into?this key period of the
出版日期Book 2018
關(guān)鍵詞Geological evolution of South Africa; Rodinia break-up; Neoproterozoic Brasiliano fold belt; Accreation
版次1
doihttps://doi.org/10.1007/978-3-319-68920-3
isbn_softcover978-3-319-88682-4
isbn_ebook978-3-319-68920-3Series ISSN 2364-6438 Series E-ISSN 2364-6446
issn_series 2364-6438
copyrightSpringer International Publishing AG, part of Springer Nature 2018
The information of publication is updating

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Geology of Southwest Gondwana978-3-319-68920-3Series ISSN 2364-6438 Series E-ISSN 2364-6446
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發(fā)表于 2025-3-22 01:24:01 | 只看該作者
Ivor Catt,David Walton,Malcolm Davidsonic data are essential to determine the paleogeographic and kinematic evolution of each Gondwana-forming block during its assembly as well as to place chronological constraints on such a process. A review of paleomagnetic data from Western Gondwana blocks indicates that the available Ediacaran to Cam
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發(fā)表于 2025-3-22 06:45:33 | 只看該作者
separated them during the assembly of Gondwana, was situated in the heart of the supercontinent. As such, the region is an ideal site to study the lithospheric structure, composition and evolution of the supercontinent. A plethora of data sets, both geological and geophysical, are available in the p
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Kia Hays,Karen Jungblut,Stephen D. Smithtic Ocean, which preserve a rich record of West Gondwana assembly and large-scale crustal evolution. Here we describe the distinct stages and tectonic regimes related to the evolution of the southern Adamastor Ocean as reconstructed from the geological record in southeastern Brazil, Uruguay and sout
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Monish R. Chatterjee,Shih-Tun Chenthe Atlantic Ocean. Some 18 geological domains of Precambrian age are distinguished in this region, covering all the geological periods from the Paleoarchean to the Neoproterozoic. An overview of the lithostratigraphy of each domain is presented, based on the most recent geochronological data. A com
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Pierluigi Malavasi,Cristian Righettiniean crustal reworking recorded in Paleoproterozoic zircon magmatic crystallization ages in widely distributed granitic orthogneisses. Supracrustal blocks of an older Neoarchean to Siderian sedimentary cover including BIFs, quartzites and marbles are preserved only as minor relics. Additionally, an i
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