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。
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.
关键词
雪峰山
波峰
构造带
找煤
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
