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河南省永城煤田山西组及下石盒子组聚煤特征

冯斌

河南理工大学学报:自然科学版2012,Vol.31Issue(2):177-181,5.
河南理工大学学报:自然科学版2012,Vol.31Issue(2):177-181,5.

河南省永城煤田山西组及下石盒子组聚煤特征

Study on coal- accumulating characteristic of Shanxi formation and low Shihezi formation in Yongcheng Coalfield,Henan province

冯斌1

作者信息

  • 1. 河南省地质矿产勘查开发局第十一地质队,河南商丘476000
  • 折叠

摘要

Abstract

Based on the theory of sedimentology and coal field geology, a systematic analysis is carried out on the sedimentary environment and coal accumulating characteristics of the lower Permian Shanxi and Lower Shi- hezi Formation in Yongcheng Coalfield of Henan province. The research shows that the sedimentary environ- ment of the lower stratum of Shanxi formation is considered as the tidal flat, and the upper stratum and the Lower Shihezi formation is the result of delta systems. The occurrence, hosting, thickness and distribution of the coal seams are controlled by depositional environment. The major ruinable coal seam Shan~ formed in peat flat of tidal flat, and its thickness is negatively correlated with the underlying sand; the coal seams of Lower Shihezi formation formed respectively in the peat swamp of construction stage and abandonment stage of delta plain.

关键词

沉积环境/聚煤特征/潮坪/三角洲

Key words

the sedimentary environment/coal accumulating characteristics/tidal flat/delta

分类

能源科技

引用本文复制引用

冯斌..河南省永城煤田山西组及下石盒子组聚煤特征[J].河南理工大学学报:自然科学版,2012,31(2):177-181,5.

基金项目

河南省国土资源厅“两权价款”地质科研项目(2011-622-10). ()

河南理工大学学报:自然科学版

OA北大核心CSTPCD

1673-9787

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