摘要
基于现有的地质和物探资料,对霍西煤田浅层地质构造重新开展了进一步的分析研究,认为霍西煤田是叠加在汾渭裂陷带上的独立构造体系,是一个典型的块内滑移地体。现存煤田是巨大滑脱体经过风化、剥蚀后的残留部分。不存在独立的“临汾新裂陷”。
Based on available geological and geophysical information, carried out further analytical study on shallow structures in the Huoxi coalfield. It is considered that Huoxi coalfield is an independent structural system superimposed on the Fenwei rift zone, a typical slip terrain within a massif. Existing coalfield is a residual fraction of huge decollement mass after weathering and denuding. Thus independent “Linfen new chasm” is not existed.
作者
罗荣贵
Luo Ronggui(The First Exploration Bureau, CNACG, Handan, Hebei 056004)
出处
《中国煤炭地质》
2019年第7期12-16,共5页
Coal Geology of China
关键词
煤田边界
裂陷
航磁异常
构造成因
霍西煤田
coalfield boundary
rift
aeromagnetic anomaly
structural genesis
Huoxi coalfield
