| 青海省北部侏罗纪煤田中的滑动构造 |
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| 引用本文： | 林文良,表哲平. 青海省北部侏罗纪煤田中的滑动构造[J]. 青海国土经略, 1996, 0(2) |
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| 作者姓名： | 林文良 表哲平 |
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| 作者单位： | 青海煤田地质研究所(林文良)，青海煤田地质研究所(表哲平) |
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| 摘 要： | 滑动构造是煤系盆地在侧向挤压形变过程中形成的一种以盆地中部物质沿着倾斜的软弱层向边部运动为特征的推覆构造。一般浅部断距较大,深部消失在软弱层中。它不同于叠瓦式逆冲构造和简单的层间滑动。
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| 关 键 词： | 滑动构造 煤系盆地 |
GLIDE TECTONICS IN JURASSIC COAL FIELD IN NORTHERN QINGHAI |
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| Lin Wenliang,Yuan Zheping Qinghai Institute of Coal Geology. GLIDE TECTONICS IN JURASSIC COAL FIELD IN NORTHERN QINGHAI[J]. QINGHAI GUOTU JINGLUE, 1996, 0(2) |
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| Authors: | Lin Wenliang Yuan Zheping Qinghai Institute of Coal Geology |
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| Affiliation: | Lin Wenliang;Yuan Zheping Qinghai Institute of Coal Geology |
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| Abstract: | The glide tectonics is such a nappe tectonics that characterized by the move-ment of materials from the centre to the margin of the basin along the dipped weak bed andformed on the synclinal basin by the lateral compression deformation. With a large faultthrow in shallow and disappearing in deep weak bed, it differ profoundly from the imbricatedthrust and simple interformation slide. |
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| Keywords: | glide tectonics coal-bearing basin |
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