| 广西弧形构造探讨 |
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| 引用本文： | 褚有龙.广西弧形构造探讨[J].地球科学,1988(6). |
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| 作者姓名： | 褚有龙 |
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| 作者单位： | 广西第七地质队 |
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| 摘 要： | 广西构造实为一弧形构造,它由四个并排的北东—北西向的轭状弧带所组成。每个弧带的前部,为坚硬的岩块所组成,所产生的断裂及岩浆活动对寻找与火成岩有关的矿产有一定意义。每个弧带的后部,产生盆地型沉积,有利于沉积矿产的形成。
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| 关 键 词： | 广西弧形构造 轭状弧带 坚硬的岩块 盆地型沉积 |
THE INVESTIGATION OF GUANGXI ARC STRUCTURE |
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| Chu Youlong.THE INVESTIGATION OF GUANGXI ARC STRUCTURE[J].Earth Science-Journal of China University of Geosciences,1988(6). |
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| Authors: | Chu Youlong |
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| Institution: | The Seventh Geological Team of Guangxi |
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| Abstract: | As a matter of fact, the structure of Guangxi is a arc structure. It is composed of four reduplicated arc zones which look like yoke and take the direction of northeast-northwest. The front of every arc zone is composed of solid rockmass.It often faults and the molten magma under it often moves.That is of significance in searching mineral resources which have something to do with igneous rocks. In the rear part of every arc zone the basin-model sedimentation occurs. It is favourable for the formation of sedimentary mineral resources. |
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| Keywords: | Guangxi arc structure yoke-like arc zone solid rockmass basin-model sedimentation |
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