内蒙古平庄盆地层序地层与聚煤规律

Sequence stratigraphy and coal-forming laws in Pingzhuang basin of Inner Mongolia

  • 摘要: 利用平庄盆地钻孔和矿井地质资料,结合野外地质调查等工作,运用沉积学、层序地层学及煤田地质学的基本理论和方法,根据古构造运动面和大面积侵蚀面,将平庄盆地含煤岩系--杏园组和元宝山组划分为1个超层序和2个层序,并把层序划分为低水位体系域(LST)、湖泊扩展体系域(LTST)、湖泊萎缩体系域(LCST)和非湖泊体系域(NLST)。总结出层序地层与聚煤规律的关系是:LST和LTST基本无聚煤作用发生;LCST局部有利地段可发育薄煤层,但无工业利用价值;NLST聚煤条件最有利,常形成厚煤层。

     

    Abstract: The sequence stratigraphy of coal measures in the Pingzhuang basin has been studied by drilling core data and field geologic survey.Applied theoretics and methods of sedimentology,sequence stratigraphy and coal geology,judged by the surface of palaeotectonics and large scale erosion surface,Xingyuan Formation and Yuanbaoshan Formation which are coal measures of Pingzhuang basin,were divided into one supersequence and two sequences;and then the sequence was subdivided into LST,LTST,LCST and NLST;the sequence of stratigraphic characteristics were expounded;at last,the relationship of sequence stratigraphy and coal-forming law were summed up.It is indicated that in the LST and LTST there is basically no coal-forming action;in the LCST locally has thin coal seams without industrial development value;the NLST has favorable coal-forming conditions,formed thick coal seams.

     

/

返回文章
返回