Geology of Southwest Gondwana

著者

書誌事項

Geology of Southwest Gondwana

Siegfried Siegesmund, Miguel Angelo Stipp Basei, Pedro Oyhantçabal, Sebastian Oriolo, editors

(Regional geology reviews)

Springer, c2018

  • : hardcover
  • : softcover

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注記

Includes bibliographical references

内容説明・目次

内容説明

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 Earth's evolution.

目次

1 The geology of key areas in the major Paleoproterozoic.- 2 The geological evolution of Southwest (SW) Gondwana.- 3 comprises parts of South America, Africa, Madagascar, Antarctica, India and Australia.- 4 Archean Cratons and Neoproterozoic Brasiliano (Pan-African) fold belts.- 5 Conclusion.

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詳細情報

  • NII書誌ID(NCID)
    BB2722729X
  • ISBN
    • 9783319689197
    • 9783319886824
  • 出版国コード
    sz
  • タイトル言語コード
    eng
  • 本文言語コード
    eng
  • 出版地
    Cham, Switzerland
  • ページ数/冊数
    xxviii, 688 p.
  • 大きさ
    29 cm
  • 親書誌ID
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