| 政和-大埔深(大)断裂带中段地质构造特征及其演化探讨 |
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| 引用本文： | 聂童春,朱根灵.政和-大埔深(大)断裂带中段地质构造特征及其演化探讨[J].福建地质,2004,23(4):186-194. |
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| 作者姓名： | 聂童春 朱根灵 |
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| 作者单位： | 福建省地质调查研究院,福州,350003;福建省地质调查研究院,福州,350003 |
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| 基金项目： | 该文是1∶25万龙岩市幅区调工作成果之一. |
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| 摘 要： | 政和—大埔深(大)断裂带为划分福建省内一级构造单元的断裂带，通过各类资料综合分析，初步认为该断裂带自中晚元古代形成以来，持续活动至今，是一条深(大)断裂带，其活动位置不断迁移，各期的构造特征也不尽相同。该断裂带的活动对其两侧地质构造格局有较大的影响，在控岩、控矿等方面具有明显的表现。
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| 关 键 词： | 深(大)断裂带 构造性质 活动特征 演化过程 政和-大埔 |
| 修稿时间： | 2004年5月10日 |
On the Characteristics and Evolution of Geological Structures in the Intermediate Section of the Zhenghe-Dapu Deep Faulted Zone |
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| Nie Tongchun,Zhu Genling.On the Characteristics and Evolution of Geological Structures in the Intermediate Section of the Zhenghe-Dapu Deep Faulted Zone[J].Geology of Fujian,2004,23(4):186-194. |
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| Authors: | Nie Tongchun Zhu Genling |
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| Abstract: | The Zhenghe-Dapu deep faulted zone is one of important faulted zones which are used to make the division of the first grade structures in Fujian Province. Based on the comprehensive study of all classes of geological information, it is preliminarily considered that the faulted zone has been active since Middle-Late Proterozoic and is a deep fracture zone. The location of its movement moves away constantly and the different stages of structural features are not in similar manner. The activity of the faulted zone exerts a biggish influence on the geological structures of both sides of this faulted zone, which makes an obvious show of the ore-control and rock-control structures. |
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| Keywords: | deep faulted zone structure characters active characteristics evolutionary process Zhenghe-Dapu area |
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