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J4 ›› 2009, Vol. 17 ›› Issue (6): 39-41.

• article • Previous Articles     Next Articles

Discussion on the Genetic Mechanism of Shizimiao An-M o Ore Field

ZHAO Riufeng，MU Xinhua   

  1. No．2 Gold Geological General Party of CAPF，Langfang   065000，Hebei，China
  • Received:2009-05-20 Revised:2009-05-26 Online:2009-12-30 Published:2011-07-15

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Abstract:

Shizimiao Au-Mo ore field is located in the middle part of Machaoying fault zone，it contains Shiyaogou nolybdenum deposit，three gold deposits such as Yuanling，Hongzhuang and Nanping．Machaoying fault zone is the main ore-controlling structure，its local pressure extending part is the main holding ore space，the mineralization closely related with intermediate acidic magmatic activity at Yanshan Period．Shiyaogou molybdenum deposit is a porphyry type molybdenum deposit controlled by blind porphyry body．The mineralization of Ag-Pb ，Au，Mo is unified with time and space，and form a holistic natural ore—form ing system．

Key words: Shizimiao, Au-Mo deposit, Genetic mechanism, Machaoying fault zone, Eastern Qinling metallogenic belt

CLC Number: 

  • P618.51


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