Jiangnan Orogen, South China: A ~970–820 Ma Rodinia margin accretionary belt
Abstract
The Neoproterozoic Jiangnan Orogen in South China records a succession of arc-trench-basin assemblages culminating in accretion of the bounding Yangtze and Cathaysia blocks to form the stabilized South China Craton. The orogen can be traced over some 1500 km and extends up to 100 km across strike. It is divisible into three domains: the northeast domain (also referred to as the Huaiyu or Shuangxiwu Terrane), the central domain (Jiuling Terrane),...
Paper Details
Title
Jiangnan Orogen, South China: A ~970–820 Ma Rodinia margin accretionary belt
Published Date
Sep 1, 2019
Journal
Volume
196
Pages
102872 - 102872
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