地震反射特征和高峰和底层煤层的起源
Rui Shan1, Ailan Nie2, Xiaoyi Cao3,4
1Coal Technology and Engineering Group Corp., Xi'an Research Institute Co., Ltd., Xi'an, 710077, China. sanxin1984@163.com.
Scientific reports
|January 30, 2026
概括
使用地震数据调查煤矿山洞和洞穴区域,发现了独特的地震反射特征. 这些发现有助于评估地下条件,并支持深层煤炭勘探.
科学领域:
- 地质物理学 地质物理学
- 采矿工程 采矿工程 采矿工程
- 地球科学 地球科学 地球科学
背景情况:
- 煤炭开采会造成山洞和洞穴区域,导致地质不稳定.
- 这种不稳定性阻碍了深层煤层的勘探和开发.
研究的目的:
- 为了调查goafs和洞穴区域的地震反射特征.
- 了解这些地震反应的起源.
- 为了将地震属性与资源勘探的底层层相关联.
主要方法:
- 使用2D迁移的地震资料.
- 在物理模型上进行地震模拟和成像.
主要成果:
- 戈夫底部显示强烈的地震反射.
- 洞穴区域表现出强烈的地震散射.
- 底层的煤层显示能量减弱,相位异常和减少连续性.
结论:
- 地震反射异常与形和洞穴区域属性有关.
- 这种相关性有助于评估goaf条件.
- 为深层煤炭资源的勘探和开发提供关键支持.
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