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REN Ji-shun. Some problems on the Kunlun-Qinling orogenic system[J]. Northwestern Geology, 2004, 37(1): 1-5.
Citation: REN Ji-shun. Some problems on the Kunlun-Qinling orogenic system[J]. Northwestern Geology, 2004, 37(1): 1-5.

Some problems on the Kunlun-Qinling orogenic system

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  • Received Date: February 19, 2004
  • Published Date: March 04, 2004
  • The Caledonian Kunlun-Qinling oceanic basin was not a successor of the Proterozoic oceanic basins, but came from a rift in the Cambrian, and was closed during the Silurian. The Carboniferous-Permian Kunlun seafloor rift or small oceanic basins had disappeared before the Late Permian. In the Triassic, there was no ocean, but just a sea in Kunlun-Qinling. Therefore, the Indosinian orogeny was not a continent-continent collision orogeny after oceanic basin disappeared, but a continent-continent superimposed orogeny(i.e. continental crust subduction one).
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