Jiangnan Orogen in South China: Developing from divergent double subduction
Abstract
null null The Jiangnan Orogen is considered as a continent–continent collisional belt resulting from the closure of a Meso-Neoproterozoic ocean separating the southeastern margin of the Yangtze Block from the northwestern margin of the Cathaysia Block. Recent data indicate the existence of early Neoproterozoic (1000–825 Ma) volcanic arc assemblages on both sides of the orogen, suggesting that the ocean lithosphere between the Yangtze and...
Paper Details
Title
Jiangnan Orogen in South China: Developing from divergent double subduction
Published Date
Apr 1, 2015
Journal
Volume
27
Issue
3
Pages
1173 - 1180
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