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福建德化汤头-大铭火山基底断隆带基本特征及控矿作用
引用本文:聂童春,陈斯盾.福建德化汤头-大铭火山基底断隆带基本特征及控矿作用[J].福建地质,2001,20(4):163-170.
作者姓名:聂童春  陈斯盾
作者单位:福建省区域地质调查队,三明,365001
摘    要:福建德化汤头-大铭火山基底断隆带位于周宁-华安火山基底断隆带的中部,以印支期的隆起-伸展构造和燕山期的地垒构造活动表现较为明显。该带构造形成及演化机制可较好诠释周宁-华安火山基底断隆带演化趋势,进一步探讨了该区域多种矿产形成及分布的规律。

关 键 词:隆起伸展构造  地垒构造  德化县  福建  控矿作用
修稿时间:2001年3月4日

On the Basic Characteristics and Ore Deposition Control of Tangtou-Daming Volcanic Basement Fault-Upwarping Belt in Dehua County, Fujian Province
Nie Dongchun,Chen Sidun.On the Basic Characteristics and Ore Deposition Control of Tangtou-Daming Volcanic Basement Fault-Upwarping Belt in Dehua County, Fujian Province[J].Geology of Fujian,2001,20(4):163-170.
Authors:Nie Dongchun  Chen Sidun
Abstract:The fault upwarping belt of Tangtou Daming volcanic basement in Dehua County, Fujian Province, located in the middle segment of the volcanic basement fault upwarping belt in the Zhouning Hua'an area, has obvious characters of Indosinian uplift extending structures and Yanshan horst structures. The formation and evolution of the structures in the fault upwarping belt were under a discussion in the paper, which can be used to explain the evolutional trend of the Zhouning Hua'an volcanic basement fault upwarping belt. And it is a great help to further analyze the formation and distribution of some minerals in the surveyed area.
Keywords:extending structure  horst structure  uplift  Dehau County  Fujian Province
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