煤田地质与勘探2011，Vol.39Issue(5)：15-17,40,4.DOI:10.3969/j.issn.1001-1986.2011.05.004
石拐盆地西段逆冲构造及找煤方向预测
Characteristics of thrust nappe structures and coal seam forecast in the western part of Shiguai basin
王怀1
作者信息
- 1. 河南省煤田地质局二队,河南 洛阳 471023
- 折叠
摘要
Abstract
In order to search for potential coal resources, by analysis of the surface and underground structure characteristics in the western part of Shiguai basin, it is considered that the front of Daqingshan thrust nappe should be F10 fault group. Surface Changhangou Formation etc. Is allochthonous strata moved 3 km away from the south. The deep main coal-bearing strata, the first member of Wudanggou Formation, is almost not affected by nappe structures. The first member of Wudanggou Formation should be more southern than its surface position. Native coal seams not effected by nappe structures should exist below Permian strata in the south of the basin.关键词
石拐盆地西段/逆冲推覆构造/原生煤层Key words
the western part of Shiguai basin/ thrust nappe/ original coal seam分类
天文与地球科学引用本文复制引用
王怀..石拐盆地西段逆冲构造及找煤方向预测[J].煤田地质与勘探,2011,39(5):15-17,40,4.
