| 雪峰山波峰构造特征及其找煤意义 |
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| 引用本文： | 方道恕.雪峰山波峰构造特征及其找煤意义[J].地球科学与环境学报,1992(1). |
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| 作者姓名： | 方道恕 |
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| 作者单位： | 江西省煤田地质科学研究所 |
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| 摘 要： | 雪峰山冲浪波峰带属于环太地壳波系,位于衡阳波谷带以西,向北西冲滑于沅水波谷带之上,可划分为冲浪波峰区、基底冲浪区、深层冲浪区、浅层冲浪区、浅层荡浪区和浅层塌浪区等六个区段。煤层主要赋存于浅层荡浪区,其次是浅层塌浪区和浅层冲浪区。
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| 关 键 词： | 雪峰山冲浪波峰带 地壳波动波基面 冲浪区 荡浪区 塌浪区 |
THE STRUCTURAL FEATURES OF THE WAVE-FRONT OF THE XUEFENG MOUNTAIN AND ITS SIGNIFICANCE FOR LOOKING FOR COAL |
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| Fang Daoshu.THE STRUCTURAL FEATURES OF THE WAVE-FRONT OF THE XUEFENG MOUNTAIN AND ITS SIGNIFICANCE FOR LOOKING FOR COAL[J].Journal of Earth Sciences and Environment,1992(1). |
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| Authors: | Fang Daoshu |
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| Institution: | Jiangxi Institute of Coal-field Geology |
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| Abstract: | The belt of the impact wave-front of the Xuefeng mountain is located to the west of the Hengyang wave-trough zone. It collides and slides toward the north- west over the wave-trough belt of the Yuan river. The impact wave-front belt of the Xuefeng mountain can be divided into six regions: impact wave-front,basal impact- wave, deep layer impact wave-front, shallow layer impact-wave, shallow layer drifting -wave and shallow layer collapse-wave. The coal seams predominantly exist in the district of the shallow layer drifting-wave and secondly in the district of the shallow layer collapse-wave. |
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| Keywords: | the belt of impact wave-front of the Xuefeng mountain wave-base of crustal undulation district of impact-wave district of drifting-wave district of collapse-wave |
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