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Geological Features of Devonian Sedimentary Basins in South China and Their Deposition and Mineralization

Geological Features of Devonian Sedimentary Basins in South China and Their Deposition and... Abstract The Devonian succession in South China is well‐known for its complete development, varified sedimentary types, remarkable lithofacies variation and abundant mineral resources. The South China plate was formed by the collision and collage of the Yangtze plate and the Cathaysian plate. The collision began approximately at the Jinningian stage and the collage was not finalized until the Guangxian movement. It was on the South China plate with a somewhat different nature of the basement that the Devonian deposition formed. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Geological Features of Devonian Sedimentary Basins in South China and Their Deposition and Mineralization

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References (2)

Publisher
Wiley
Copyright
© 1994 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.1994.mp7001005.x
Publisher site
See Article on Publisher Site

Abstract

Abstract The Devonian succession in South China is well‐known for its complete development, varified sedimentary types, remarkable lithofacies variation and abundant mineral resources. The South China plate was formed by the collision and collage of the Yangtze plate and the Cathaysian plate. The collision began approximately at the Jinningian stage and the collage was not finalized until the Guangxian movement. It was on the South China plate with a somewhat different nature of the basement that the Devonian deposition formed.

Journal

Acta Geologica Sinica (English Edition)Wiley

Published: Mar 1, 1994

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