GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 会议论文
湘东北连云山地区晚中生代的变形特征与构造意义
叶挺威; 许德如; 陈根文; 王智琳; 于得水
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 Date2017-12-09
Conference Place中国江西南昌
Country中国
Indexed By其他
Language中文
Keyword晚中生代 湘东北 变形特征 新元古代地层 冷家溪群
Abstract连云山地区位于江南造山带湖南段的北东部(即湘东北)。该区出露的地层主要为新元古界冷家溪群和板溪群,还有少量的泥盆系和白垩系,以及第四系盖层。区内主要控矿构造为长沙-平江深大断裂(简称长平断裂),是华南地区晚中生代伸展构造型式的重要组成部分。断裂带两侧岩性存显著差异,其东南侧为新元古代冷家溪群和晚中生代连云山岩体(U-Pb年龄145Ma;许德如等,2017),井冲、横洞钴铜矿床和
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35620
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
叶挺威,许德如,陈根文,等. 湘东北连云山地区晚中生代的变形特征与构造意义[C],2017.
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