| 福建安溪铅山铅锌矿区复成分角砾岩地层特征及成因探讨 |
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| 引用本文： | 佘日启.福建安溪铅山铅锌矿区复成分角砾岩地层特征及成因探讨[J].福建地质,2007,26(3):151-161. |
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| 作者姓名： | 佘日启 |
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| 作者单位： | 福建省闽东南地质大队,泉州,362011 |
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| 摘 要： | 安溪铅山铅锌矿区复成分角砾岩为一套火山碎屑岩-沉火山碎屑岩-火山碎屑沉积岩。形成时代拟归三叠世文宾山组。为滨海-海陆交互相地层。
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| 关 键 词： | 复成分角砾岩 地层特征、成因探讨 安溪铅山 |
| 收稿时间： | 2007-04-27 |
Discussion on the Genesis and Characteristics of Polymictic Breccia Strata in the Qianshan Lead-zinc Ore District of Anxi County, Fujian Province |
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| She Riqi.Discussion on the Genesis and Characteristics of Polymictic Breccia Strata in the Qianshan Lead-zinc Ore District of Anxi County, Fujian Province[J].Geology of Fujian,2007,26(3):151-161. |
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| Authors: | She Riqi |
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| Institution: | Southeastern Fujian Geological Party of Fujian Province,Quanzhou,362011 |
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| Abstract: | The polymictic breccia in the Qianshan lead-zinc ore district of Anxi County is a suit of volcaniclastic rock,sedimentary pyroclastic rock and pyroclastic sedimentary rock.It is inferred that the formation time of the polymictic breccia is Triassic Wenbishan Formation.And it is the strata of an offshore,continent and sea alternant phase. |
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| Keywords: | polymictic breccia stratum characteristics genesis discussion Anxi County |
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