| 福建大田建爱地区多金属矿的构造特征及其成矿意义 |
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| 引用本文： | 黄长煌.福建大田建爱地区多金属矿的构造特征及其成矿意义[J].福建地质,1999,18(1):6-11. |
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| 作者姓名： | 黄长煌 |
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| 作者单位： | 闽西地质大队!三明，365001 |
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| 摘 要： | 通过对研究区域构造发展史的概述和斑岩型，似层状多金属矿的构造特征论述，试图说明斑岩型，似层状热液型多金属矿受燕山晚期造山带菜构造的控制，并提出了成矿的构造模式。
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| 关 键 词： | 伸展构造 多金属矿 成矿模式 矿床构造 福建 |
Structural Characteristics and Ore forming Signification of the Multimetal Deposit in Jianai District,Datian County, Fujian Province |
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| Huang,Changhuang.Structural Characteristics and Ore forming Signification of the Multimetal Deposit in Jianai District,Datian County, Fujian Province[J].Geology of Fujian,1999,18(1):6-11. |
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| Authors: | Huang Changhuang |
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| Abstract: | According to the regional tectonic evolution of the surveyed area and the structural characteristics of the porphyry and stratoid multimetal deposit,the authors tried in the paper to explain that the distribution of stratoid,hydrothermal and porphyry multimetal deposit was controlled by the extensional structures of Late Yanshanian Orogenic Belt,and presented a metallogenic pattern of the deposit. |
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| Keywords: | extensional structure multimetal deposit metallogenic pattern Datian County Fujian Province |
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