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Geological Society of China

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    LI Fu-dong, ZOU Xiang-hua, GAO Ji-pu, et al. On the rapid-positioning and prediction for micro-dissemination type (sedimentary rock host) gold deposit (ore bodies), Ma’anqiao[J]. Northwestern Geology, 2001, 34(1): 27-63.
    Citation: LI Fu-dong, ZOU Xiang-hua, GAO Ji-pu, et al. On the rapid-positioning and prediction for micro-dissemination type (sedimentary rock host) gold deposit (ore bodies), Ma’anqiao[J]. Northwestern Geology, 2001, 34(1): 27-63.

    On the rapid-positioning and prediction for micro-dissemination type (sedimentary rock host) gold deposit (ore bodies), Ma’anqiao

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    • Received Date: June 17, 2000
    • Revised Date: November 19, 2000
    • Published Date: March 04, 2001
    • Ma'anqiao gold deposit is one of mast important gold deposits, occurring in sedimentary strata, in the middle-west part of Qinling——"Central Orogen", China and reaches into a large scale in reserves; and its potential of resources adds year after year. The gold deposit has typical significance in the metallogenic mechanism and evolutionary pattern and can be compared with well known gold deposits of the samp type at home and abroad. Major achievements of the study are as follows.
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      张复新,等. 马鞍桥金矿成矿地质条件及矿床成因[J]. 地质找矿论丛, 1997,12(1).
      隗合明. 周至马鞍桥金矿床成矿控制条件及找矿标志[J]. 西安地质学院学报,1997,19(4).
      孟庆任,等.秦岭商丹带内黑河地区砾岩沉积及其构造意义[J].沉积学报,1994,12(3).
      孟庆任,等.北秦岭南缘弧前盆地沉积作用及盆地发展[J].地质科学,1997,(2).
      曹思魁.陕西商州龙庙、周至马鞍桥铜黝银矿矿物特征研究[J].地质实验室,1997,(1).
      卢武长.稳定同位素地球化学[M].成都:成都地质学院出版社,1986.
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