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ZHANG Han-wen. Mineralized feature, tectonic setting and metallogenic type of Tongyugou cupper deposit, Qinghai province[J]. Northwestern Geology, 2001, 34(4): 30-42.
Citation: ZHANG Han-wen. Mineralized feature, tectonic setting and metallogenic type of Tongyugou cupper deposit, Qinghai province[J]. Northwestern Geology, 2001, 34(4): 30-42.

Mineralized feature, tectonic setting and metallogenic type of Tongyugou cupper deposit, Qinghai province

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  • Received Date: September 23, 2001
  • Published Date: December 04, 2001
  • Tongyugou cupper deposit located at the Triassic sedimentary basin of Hainai (to the South of Qinghai Lake) occures in a olistostrome felt with E-W orientation and in the transitional position from marene sedimentary series to volcanic-sedimentary series, which is characterized by typical dedded or ebodies and association with wrigglites and silicon-rich sedimentary rocks.On the basis of the sedimentary formation, sedimentary facies of ore-bearing series and the nature of the volcanic rocks, the tectonic setting of the deposit is considered to be spreading-subsidence basin existting in continental margin.The contrast to different stratiform sulfide deposits indicate Tongyugou depositis between Sedex type and Besshi type but closer to the latter.
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