Development and Prototype Features of Evolution in the Yangtze Basin

Abstract:

The marine sedimentary basin evolution was developed from Jinning movement in the Yangtze and the peripheral region. The continental basin had generated in Middle and Late Triassic. In the Late Proterozoic Early Paleozoic, the tectonic evolution of the phase development and evolution of the basin could be divided into three stages, namely Qingbaikou-Early Sinian, Late Sinian Middle Ordovician, and Late Ordovician Blog Silurian. Three important stages of evolution were Devonian-Early Carboniferous, Late Carboniferous-Early Permian, and Late Permian-Middle Triassic in Late Paleozoic-Mesozoic. Ancient southern continent of Asia had been further proliferation as the Indosinian movement in Middle and Late Triassic.

• Periodical: Applied Mechanics and Materials (Volumes 522-524)
• Pages: 1249-1253
• DOI: https://doi.org/10.4028/www.scientific.net/AMM.522-524.1249
• Online since: February 2014
• Authors: Yuan Yuan*, Zong Ting Liao
• Keywords: Jinning Movement, Tectonic Evolution

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