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SONG Zhong-bao, CHEN Xiang-yang, REN You-xiang, et al. Petroregimentation,Petrochemistry and Geologic Meaning of “Carbonaceous (Gritstone) Slabstone” in Deerni Deposit,Eastern Kunlun Area, Northwest China[J]. Northwestern Geology, 2008, 41(4): 77-81.
Citation: SONG Zhong-bao, CHEN Xiang-yang, REN You-xiang, et al. Petroregimentation,Petrochemistry and Geologic Meaning of “Carbonaceous (Gritstone) Slabstone” in Deerni Deposit,Eastern Kunlun Area, Northwest China[J]. Northwestern Geology, 2008, 41(4): 77-81.

Petroregimentation,Petrochemistry and Geologic Meaning of “Carbonaceous (Gritstone) Slabstone” in Deerni Deposit,Eastern Kunlun Area, Northwest China

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  • Received Date: January 01, 2008
  • Revised Date: March 25, 2008
  • Published Date: December 04, 2008
  • The Deerni Co-Cu depositis mainly formed by submarine exhalative-sedimentation,which is also charact erized by late-stage superimposed mineralization.According to petroregimentation and petrochemistry,"carbonaceous slabstone" in Deerni deposit may be divided into two categories: carbonaceous Al-Si slabstone and carbonaceous Fe-Si rock.The later is hydrothermal sedimentary rocks and the hydrothermal sedimentary rocks have formed deposit.Therefore,it is part of the outcome of Deerni mineralization.
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