GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 会议论文
西昆仑阿克萨依铁矿矿床特征及地质意义
董瑞; 王核; 张晓宇; 魏小鹏; 李沛
Source Publication中国矿物岩石地球化学学会第九次全国会员代表大会暨第16届学术年会文集
2017-04-18
Conference Date2017-04-18
Conference Place中国陕西西安
Country中国
Indexed By其他
Language中文
Keyword铁矿 阿克 巴勒斯坦 大红柳滩 西昆仑
Abstract西昆仑阿克萨依矿区大地构造位置位于康西瓦结合带南侧,地处巴颜喀拉晚古生代-中生代北缘裂陷带西端北侧,即所谓"巴颜喀拉-松潘甘孜三叠纪增生地体"。区内韧性剪切带、剥离断层、北西向脆韧性逆冲断裂及其与之有关的次级断裂发育,长轴延伸与区域构造线方向一致的侵入体广泛分布,岩浆期后热液活动频繁,构造控矿特征明显(丁道桂,1996)。
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35580
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
董瑞,王核,张晓宇,等. 西昆仑阿克萨依铁矿矿床特征及地质意义[C],2017.
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