| 广东二叠纪区域构造背景及聚煤古构造因素 |
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| 引用本文： | 张德民.广东二叠纪区域构造背景及聚煤古构造因素[J].中国煤田地质,1995,7(4):26-31. |
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| 作者姓名： | 张德民 |
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| 作者单位： | 广东煤田地质局 |
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| 摘 要： | 根据板块活动论以及华南区域构造研究的最近进展，分析了广东二叠纪的区域构造背景及聚煤古构造因素。认为广东二叠纪煤系沉积在华南板块上，古特提斯的演化（开合律）、华南板块上茅口期的裂陷作用以及中、晚二叠世之交的钦州运动决定和影响着广东二叠纪的聚煤作用。
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| 关 键 词： | 古特提斯 构造背景 二叠纪 古构造 聚煤 煤系 |
THE REGIONAL TECTONIC BACKGROUND AND PALAEO SIRUCTURE FACTORS OF COAL ACCUMULATION DURING PERMIAN IN GUANGDONG |
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| Zhang Demin.THE REGIONAL TECTONIC BACKGROUND AND PALAEO SIRUCTURE FACTORS OF COAL ACCUMULATION DURING PERMIAN IN GUANGDONG[J].Coal Geology of China,1995,7(4):26-31. |
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| Authors: | Zhang Demin |
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| Abstract: | According to the plate active theory and the latest study of Huanan regional tec-tonia,this paper analyzed regional tectonic background and palaeostructure factors of Permi-an coal accumulation in Guangdong,It is considered that Guangdong Permian coal-bearingseries deposited on Huanan plate,and the coalaccumulation is determined by the evolution ofPalaeo-Tethys,the rifting during Maokou Period on Huanan-plate and Qingzhou-move-ment between Late Permian and Middle Permian. |
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| Keywords: | Paileo-Tethys Huanan plate ri-fiting Qingzhou-movement Permian palaeo structure |
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