胡受权,郭文平.滇西北宁蒗地区树扎—树劳河一带华力西期基性喷出岩系含矿性研究[J].地质找矿论丛,1995,(3):43-49
滇西北宁蒗地区树扎—树劳河一带华力西期基性喷出岩系含矿性研究
STUDY ON ORE-BEARING PROPERTY OF VARISCAN BASIC EXTRUSIVES FROM SHUZA TO SHULAOHE IN NINGLANG AREA OF NORTHWEST YUNNAN
投稿时间:1995-03-15  修订日期:1995-05-16
DOI:10.6053/j.issn.1001-1412.1995.3. 005
中文关键词:  宁蒗地区  华力西期  基性喷出岩系  含矿性
英文关键词:
基金项目:
作者单位
胡受权 成都理工学院, 成都, 610059 
郭文平 四川盐业地质钻井大队, 自贡, 643000 
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中文摘要:
      研究区华力西期基性喷出岩系具明显的旋回性和韵律性,属滨-浅海相喷发-沉积环境。随着区内华力西期基性岩浆演化分异作用的进行,其含矿性(铜、铅、锌等)呈现递增的变化规律。第Ⅲ、Ⅳ旋回玄武岩系(P3和P2h)是区内重要的矿源层和赋矿层位。
英文摘要:
      Variscan basic extrusives with distinct cyclicity erupted and deposited from littoral region to epeiric sea during variscan period. In pace with the Variscan basic maginatic differentitation, its ore-bearing property (meaning content of Cu、Pb、Zn etc) is progressively increasing. The basaltic formation of the third and fourth cycle (P3 and P2h)is the important ore Source and ore bed in this district.
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