湘东北地区燕山期伸展构造与铅锌多金属成矿关系研究

	湘东北地区燕山期伸展构造与铅锌多金属成矿关系研究
	于得水; 朱昱桦; 叶挺威; 赵朝霞; 陈根文; 许德如
Source Publication	第八届全国成矿理论与找矿方法学术讨论会论文摘要文集
	2017-12-09
Conference Date	2017-12-09
Conference Place	中国江西南昌
Country	中国
Indexed By	其他
Language	中文
Keyword	伸展构造湘东北燕山期剥离断层成矿关系
Abstract	湘东北地区位于江南造山带中段,属于扬子地块与华夏地块的过渡地带,是我国重要的金属成矿带。区内的桃林、栗山铅锌多金属矿床,规模很大,其中桃林铅锌矿自南西向北东依次可划分为6个矿段:断山、官山、上塘冲、银孔山、杜家冲和邱坪坳。研究区内的地层主要为冷家溪群的浅变质岩(板岩、千枚岩、石英岩、片岩等)和白垩纪-第三纪红层(砾岩、砂岩);区内构造主要为北东向的石田畈断裂,其为邱坪坳-石田畈入字型构造的南西段;岩浆岩主要
Document Type	会议论文
Identifier	http://ir.gig.ac.cn/handle/344008/35621
Collection	中国科学院矿物学与成矿学重点实验室
Recommended Citation GB/T 7714	于得水,朱昱桦,叶挺威,等. 湘东北地区燕山期伸展构造与铅锌多金属成矿关系研究[C],2017.

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