| 广东箭竹洋锡铅锌多金属矿区地质特征及成因初探 |
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| 引用本文： | 李表鹏,胡文杰,朱沛云,陈彦煜,莫建永. 广东箭竹洋锡铅锌多金属矿区地质特征及成因初探[J]. 资源环境与工程, 2020, 34(2): 207-209. DOI: 10.16536/j.cnki.issn.1671-1211.2020.02.008 |
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| 作者姓名： | 李表鹏 胡文杰 朱沛云 陈彦煜 莫建永 |
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| 作者单位： | 广东省有色金属地质局 九三一队,广东 汕头 515041,广东省有色金属地质局 九三一队,广东 汕头 515041,广东省有色金属地质局 九三一队,广东 汕头 515041,广东省有色金属地质局 九三一队,广东 汕头 515041,广东省有色金属地质局 九三一队,广东 汕头 515041 |
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| 摘 要： | 广东箭竹洋地区位于武夷成矿带南段、莲花山断裂带南西段,经1∶50000龙村圩幅地质填图中D6540、D6543等地质观察点、槽探工作及民窿调查发现3条锡铅锌矿化体V 1、V 2、V 3,矿化体赋存于灰黑色凝灰质板岩与花岗岩接触带中,走向受北东向韧性剪切带控制,推断矿床成因属于岩浆热液改造型锡多金属矿床,为粤东进一步的找矿工作提供了指示性意义。
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| 关 键 词： | 锡铅锌 岩浆热液改造型 莲花山 广东箭竹洋 |
Geological Characteristics and Genesis of Tin-Lead-Zinc Polymetallic Mining Area in Jianzhuyang,Guangdong Province |
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| Li Biaopeng,Hu Wenjie,Zhu Peiyun,Chen Yanyu,Mo Jianyong. Geological Characteristics and Genesis of Tin-Lead-Zinc Polymetallic Mining Area in Jianzhuyang,Guangdong Province[J]. Resources Environment & Engineering, 2020, 34(2): 207-209. DOI: 10.16536/j.cnki.issn.1671-1211.2020.02.008 |
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| Authors: | Li Biaopeng Hu Wenjie Zhu Peiyun Chen Yanyu Mo Jianyong |
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| Affiliation: | (Team of Guangdong Nonferrous Metals Geological Bureau,Shantou,Guangdong 515041) |
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| Abstract: | The Jianzhuyang area in Guangdong Province is located in the southern part of the Wuyi metallogenic belt and the southern and western part of the Lianhuashan fault zone.Three tin-lead-zinc mineralizations,V 1,V 2 and V 3,are found in the 1∶50000 geological mapping,such as D6540 and D6543.The mineralizations occur in the contact zone between grey-black tuffaceous slate and granite,and their strike is controlled by the NE-trending ductile shear zone.As it belongs to the magmatic hydrothermal reformed tin polymetallic deposit,it provides an indication for further prospecting work in eastern Guangdong. |
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| Keywords: | Tin-lead-zinc magmatic hydrothermal transformation type Lianhuashan Jianzhuyang of Guangdong |
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