ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
金平地区超基性岩铜镍矿床成矿作用类型及找矿方向
  
关键词:magmatic copper-nickel deposit  mineral deposit geology  mineralization  geology and ore-prospecting  Jinping in Yunnan
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徐金祥 云南省有色地质局三〇六队 ynxujx308@126.com 
陈春 云南省有色地质局三〇六队  
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摘要:
Metallogenic Types and Ore-prospecting Orientations of Ultrabasic Rock Copper-nickel Deposits in Jinping Area
      The Jinping basic-ultrabasic rock belt in the southeastern part of the Dali-Yuanjiang-Jinping mafic and ultramafic rock belt can be further divided into three sublets. The Baimazhai-Xin’anli ultrabasic rock subbelt and the Niulanchong-Jiangjiaping basic-ultrabasic rock subbelt are characterized by high degree of basic-ultrabasic magmatic differentiation, intense copper and nickel mineralization, and multi-stage and multi-phase rock-forming and ore-forming activities. Typical ore-forming activities of copper-nickel deposits in the study area include such types as liquation-emplacement-injection type and emplacement-liquation type. Baimazhai-Xin’anli district and Niulanchong-Jiangjiaping district constitute the central places of ultramafic magmatic intrusion and copper-nickel mineralization in Jinping area, and are also important targets in further geological and ore-prospecting work.
XU Jin-xiang,CHEN Chun.2013.Metallogenic Types and Ore-prospecting Orientations of Ultrabasic Rock Copper-nickel Deposits in Jinping Area[J].Acta Geoscientica Sinica,34(s1):101-107.
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