宁夏海原西华山地区金矿床地质地球化学特征及成因分析
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苏力 1( ),朱海军 1,谷守江 1( ),杨兴科 2( ),赵翌辰 2,孙雪平 1,何虎军 2,韩珂 2,张玉瑜 1,谭江 1,谢愿龙 1,张龙 1,高立博 1
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Geological and Geochemistry Characteristics and Genesis Analysis of Gold Deposits in Xihuashan Area,Haiyuan,Ningxia
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Li SU 1( ),Haijun ZHU 1,Shoujiang GU 1( ),Xingke YANG 2( ),Yichen ZHAO 2,Xueping SUN 1,Hujun HE 2,Ke HAN 2,Yuyu ZHANG 1,Jiang TAN 1,Yuanlong XIE 1,Long ZHANG 1,Libo GAO 1
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图1. 宁夏海原南西华山铜金矿区构造单元(张海波等,2016) Ⅰ-阿拉善—华北地块;Ⅰ-1-阿拉善地块;Ⅰ-2-鄂尔多斯地块;Ⅰ-3-贺兰裂陷槽;Ⅱ-阿拉善—华北地块南缘;Ⅱ-1-走廊弧后盆地;Ⅱ-2-走廊南山岛弧;Ⅱ-3-北祁连缝合带;Ⅲ-柴达木地块;Ⅳ-秦岭造山带;1.断裂;2.黄河;3.研究区
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Fig.1. Tectonic unit of Nan-Xihuashan copper-gold district in Haiyuan of Ningxia(Zhang et al.,2016)
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