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SONG Zhong-bao, JIA Qun-zi, ZHANG Zhan-yu, et al. Study on Geological Feature and Origin of Yemaquan Fe-Cu Deposit in Qimantage Area,Eastern Kunlun[J]. Northwestern Geology, 2010, 43(4): 209-217.
Citation: SONG Zhong-bao, JIA Qun-zi, ZHANG Zhan-yu, et al. Study on Geological Feature and Origin of Yemaquan Fe-Cu Deposit in Qimantage Area,Eastern Kunlun[J]. Northwestern Geology, 2010, 43(4): 209-217.

Study on Geological Feature and Origin of Yemaquan Fe-Cu Deposit in Qimantage Area,Eastern Kunlun

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  • Received Date: October 19, 2010
  • Revised Date: November 23, 2010
  • Published Date: December 04, 2010
  • The genesis of Yemaquan iron-polymetallic deposit was defined as skarn-type.The author found appearance of exhalative rock and jasper rock on the top of ore deposit which give evidence to exhalative-sedimentary mineralization.By analysis of comparison,the author considered that there is exhalative-sedimentary mineralization on the early stage,and on the later stage is skarn-type mineralization,so the orig in of Yem aquan Fe-Cu deposit should be exhalative-sedimentary and skarn-type.This may have some importance in theory on prospect in Qimantage region.
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