| 福建莆田泗洋铅锌矿地质特征及成因探讨 |
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| 引用本文： | 梁乐辉.福建莆田泗洋铅锌矿地质特征及成因探讨[J].福建地质,2008,27(3):259-266. |
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| 作者姓名： | 梁乐辉 |
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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： | 泗洋铅锌矿产于南园组第三段中酸-酸性火山碎屑岩中，矿体呈透镜状、脉状，受断裂构造、火山环状构造控制。成矿与中生代岩浆侵入及火山活动紧密相关，为中低温岩浆-火山热液型矿床。
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| 关 键 词： | 铅锌矿 地质特征 成因探讨 莆田泗洋 |
Discussion on the Geologic Characteristics and Genesis of the Siyang Lead-zinc Deposit in Putian City, Fujian Province |
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| Liang Lehui.Discussion on the Geologic Characteristics and Genesis of the Siyang Lead-zinc Deposit in Putian City, Fujian Province[J].Geology of Fujian,2008,27(3):259-266. |
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| Authors: | Liang Lehui |
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| Institution: | Liang Lehui (Southeastern Geology Party of Fuj ian Province, Quanzhou , 362011) |
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| Abstract: | The Siyang lead-zinc deposit is discovered in the intermediate acid and acidic volcanoclastic rock of the Late Jurassic Nanyuan Formation.The orebody,with a lenticular or veiny form,is controlled by the faulted structures and volcano ring structures.The metallogenesis of the deposit has a close relation with Mesozoic magmatic intrusion and volcanic activity.It belongs to the deposit of intermediate and low temperature magmatic and volcanic hydrothermal type. |
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| Keywords: | lead-zinc ores geologic characteristics genesis Putian City |
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