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Meso-Cenozioc Tectonic Attribute of Southern China and Folding of the Nanhua (South Cathay) Orogenic Belt |
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| Authors: | GUO FuxiangResearch Centre of Prediction of Hidden Ore Deposits Guilin Institute of Technology Guilin Guangxi Wang Yi Fei Zhenbi |
| Abstract: | The Meso-Cenozoic tectonic attribute of southern China is a continental tridirectional orogenic belt formed by subsynchronous interaction among the Tethys, Northwest Pacific and Kunlun-Qinling tectonic domains. It was created by superimposition of repeated orogenies since the Late Permian. The Indosinian folds therein are gentle and localized. |
| Keywords: | continental tridirectional -erogenic belt platform cover Indosinian orogeny Meso-Cenozoic southern China |
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