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开平-涧河地区山西组的沉积与聚煤研究

Deposition and Coal Accumulation of Shanxi Formation in Kaiping-Jianhe Area

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【作者】 沙亚南张宏郭英海李壮福张天模

【Author】 SHA Ya-nan; ZHANG Hong ; GUO Ying-hai ; LI Zhuang-fu ; ZHANG Tian-mo(Jiangsu Bureau of Coal Geology, Changzhou, Jiangsu 510440, China ; Kailuan Mining Bureau, Tangshan, Hebei 510440, China ; College of Mineral Resource and Environment Sciences, CUMT, X

【机构】 江苏煤田地质局!江苏常州217013开滦矿务局!河北唐山063000中国矿业大学资源与环境科学学院!江苏徐州221008重庆工程技术学校!重庆400037

【摘要】 研究了开平-涧河地区主要含煤地层之一─—山西组的沉积特征,介绍了山西组沉积演化特点,提出了山西组为受海泛作用影响的浅水三角洲沉积,指出聚煤作用及煤层展布主要受沉积环境控制,与海侵密切相关,认为聚煤作用主要形成于废弃三角洲及三角洲间湾充填变浅背景上发育起来的泥炭沼泽环境。

【Abstract】 Shanxi Formation is one of the main coal-bearing strata in Kaiping-Jianhe area. The field and laboratory studies show that Shanxi Formation is a shallow water delta deposition mainly influenced by ingression. The sedimentary evolution of Shanxi Formation was discussed. Coal accumulation and coal bed distribution were controlled by sedimentary environment and were closely related to regression. Coal accumulation occurred mainly in the peat swamps developed on the base of abandoned delta and filling-shallowed delta distributary bay.

  • 【文献出处】 中国矿业大学学报 ,JOURNAL OF CHINA UNIVERSITY OF MINING & TECHNOLOGY , 编辑部邮箱 ,2000年02期
  • 【分类号】P512.3
  • 【被引频次】6
  • 【下载频次】138
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