摘要
在野外地表观察描述和深部钻探取心编录研究的基础上,对贺兰山南段新井盆地煤炭沉积环境与聚煤作用进行分析。结果发现,新井盆地含煤地层主要是下—中侏罗统延安组,在沉积环境上属冲积扇-河流相环境体系;含煤地层受古构造、古地理等多种因素的影响和控制,在山麓沉积与曲流河沉积带之间形成了盆地内工业煤层和富煤中心。
Based on the study of field surface observation and deep borehole compaction, a brief analysis of the coal depositional environment and coal accumulation in the Xinjing Basin of the southern Helan Mountain Basin was carried out. The coal-bearing strata in the Xinjing Basin are mainly distributed in the middle-lower Jurassic Yan 'an Formation, which is an alluvial fan-river face system in the sedimentary environment. The coal-bearing strata are influenced and controlled by various factors such as paleo-tectonics and palaeogeography. Between the foothills and the sedimentary belt of the meandering river,the industrial coal seam and the rich coal center are formed in the basin.
引文
[1]陈钟惠.含煤岩系沉积环境分析[M].北京:地质出版社,1984:62-63.