GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
豫西祁雨沟矿区189矿体流体包裹体研究及其对找矿的指示意义
齐楠; 陈衍景; 邓轲; 王玭; 许强伟; 方京; 疏孙平; 周振菊
Source Publication2017中国地球科学联合学术年会论文集(四十九)——专题102:大火成岩省与资源环境响应、专题103:矿田构造与区域成矿
2017-10-15
Conference Date2017-10-15
Conference Place中国北京
Country中国
Indexed By其他
Language中文
Keyword流体包裹体 水溶液包裹体 祁雨沟 均一温度 成矿阶段
Abstract祁雨沟矿区地处华北板块南缘,区内金属矿产资源丰富。区域出露地层从下到上分别是太古宇-元古宇太华群、中元古界长城系熊耳群和新生界的古近系、新近系、第四系沉积物。太华群为一套长英质片麻岩和表壳岩系夹超基性-基性变质岩系组成,主要岩性有黑云斜长片麻岩、混合片麻岩和斜长角闪岩,是区内爆破角砾岩型矿体的主要围岩。熊耳群展布于区域东部和南部,整合于太华群之上,
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35603
Collection中国科学院矿物学与成矿学重点实验室
Recommended Citation
GB/T 7714
齐楠,陈衍景,邓轲,等. 豫西祁雨沟矿区189矿体流体包裹体研究及其对找矿的指示意义[C],2017.
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