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白马寨铜镍硫化矿地球化学特征及成矿
引用本文:宋立军,吴冲龙,朱杰勇,尹潘,梁雄兵,张中旺,佟彦明.白马寨铜镍硫化矿地球化学特征及成矿[J].地质与勘探,2005,41(4):39-46.
作者姓名:宋立军  吴冲龙  朱杰勇  尹潘  梁雄兵  张中旺  佟彦明
作者单位:1. 中国地质大学,武汉,430074
2. 昆明理工大学,昆明,650093
3. 中国地质大学,武汉,430074;湖北襄樊学院,襄樊,441053
摘    要:系统研究金平县白马寨铜镍硫化矿地质、矿床地球化学特征,初步认为该矿床形成于华力西期弧后盆地拉张的构造环境.并提出本矿床为幔源岩浆熔离-结晶分异,岩浆、含矿岩浆、富矿岩浆和矿浆依次脉冲式贯入成矿和成矿期后煌斑岩浆侵入破坏,并叠加成矿的矿床成因模式.从而,建立了本区铜镍矿床的成矿模型,并对该矿床深部及外围找矿提出建议.

关 键 词:地球化学  成矿环境  成矿模式  白马寨
文章编号:0495-5331(2005)04-0039-08
收稿时间:2004-10-11
修稿时间:2004年10月11

GEOCHEMICAL CHARACTERISTICS AND MINERALIZATION OF BAIMAZHAI CU-NI SULFIDE DEPOSIT, YUNNAN PROVINCE
SONG Li-jun,WU Chong-long,ZHU Jie-yong,YIN Pan,LIANG Xiong-bing,ZHANG Zhong-wang,Tong Yan-ming.GEOCHEMICAL CHARACTERISTICS AND MINERALIZATION OF BAIMAZHAI CU-NI SULFIDE DEPOSIT, YUNNAN PROVINCE[J].Geology and Prospecting,2005,41(4):39-46.
Authors:SONG Li-jun  WU Chong-long  ZHU Jie-yong  YIN Pan  LIANG Xiong-bing  ZHANG Zhong-wang  Tong Yan-ming
Abstract:Based on systemic studies of geology and geochemistry characteristics of Baimazhai Cu-Ni deposit in Jinping county, Yunnan province, it is suggested that the Baimazhai ore deposit was formed in Variscan post-arc extensional environment of continent margin. An ore-forming model with fractional crystallization of mantle-derived magma melt-crystal difference, magma, ore-bearing magma, ore-rich magma, ore-magma pulsed inrush in turn, post-mineralization lamprophyre magma intrusion and superposition mineralization has been proposed. Ore-forming model of the Cu-Ni deposit is established and exploration suggestions at the periphery and deep part of deposit are pointed out.
Keywords:geochemistry  ore-forming environment  ore-forming model  Baimazhai
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