| 华南泥盆纪的沉积盆地特征沉积作用和成矿作用 |
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| 引用本文： | 刘文均,张锦泉.华南泥盆纪的沉积盆地特征沉积作用和成矿作用[J].地质学报,1993,67(3):244-254. |
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| 作者姓名： | 刘文均 张锦泉 |
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| 作者单位： | 成都地质学院，成都地质学院，成都地质学院 |
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| 摘 要： | 华南地区泥盆系以其发育齐全、沉积类型多样、岩相变异显著和矿产资源丰富而著称,它是由扬子板块和华夏板块碰撞拼合而成,碰撞时间大约始于晋宁期,而到广西运动之后最终拼合。泥盆纪沉积就发生在这个基底性质有所不同的华南板块之上。
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| 关 键 词： | 泥盆纪 沉积盆地 成矿作用 |
GEOLOGICAL FEATURES OF DEVONIAN SEDIMENTARY BASINS IN SOUTH CHINA AND THEIR DEPOSITION AND MINERALIZATION |
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| Liu Wenjun,Zhang Jinquan and Chen Hongde.GEOLOGICAL FEATURES OF DEVONIAN SEDIMENTARY BASINS IN SOUTH CHINA AND THEIR DEPOSITION AND MINERALIZATION[J].Acta Geologica Sinica,1993,67(3):244-254. |
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| Authors: | Liu Wenjun Zhang Jinquan and Chen Hongde |
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| Affiliation: | Chengdu College of Geology |
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| Abstract: | The Devonian sedimentary basins are developed in the unified South China plate. According to their tectonic settings, sedimentationa' features and formation mechanisms, they can divided into intercontinental and epicontinental types, and subdivided into d |
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| Keywords: | Devonian features of sedimentay basins mineralization South China |
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