GYIG OpenIR  > 矿床地球化学国家重点实验室  > 期刊论文
陕西铜厂矿田控矿断裂带显微构造特征
韩润生; 朱大岗; 马德云; 马更生; 刘伟
2000
Source Publication地质地球化学
Issue1Pages:28-33
Keyword显微构造 动力成岩成矿作用 古应力值 铜厂矿田 陕西
Subject Area矿床地球化学
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7198
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
韩润生,朱大岗,马德云,等. 陕西铜厂矿田控矿断裂带显微构造特征[J]. 地质地球化学,2000(1):28-33.
APA 韩润生,朱大岗,马德云,马更生,&刘伟.(2000).陕西铜厂矿田控矿断裂带显微构造特征.地质地球化学(1),28-33.
MLA 韩润生,et al."陕西铜厂矿田控矿断裂带显微构造特征".地质地球化学 .1(2000):28-33.
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