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开平-涧河地区山西组的沉积与聚煤研究
引用本文:沙亚南,张宏,郭英海,李壮福,张天模. 开平-涧河地区山西组的沉积与聚煤研究[J]. 中国矿业大学学报, 2000, 29(2): 203-206
作者姓名:沙亚南  张宏  郭英海  李壮福  张天模
作者单位:1. 江苏煤田地质局, 江苏常州 217013
2. 开滦矿务局,河北唐山 063000;
3. 中国矿业大学资源与环境科学学院,江苏徐州 221008
4. 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放间湾充填变浅背景上发育起来的泥炭沼泽环境。

关 键 词:聚煤 海浸 山西组 开平-涧河地区 沉积 煤矿床
文章编号:1000-1964(2000)02-0203-04
修稿时间:1999-09-27

Deposition and Coal Accumulation of Shanxi Formation in Kaiping-Jianhe Area
SHA Ya-nan, ZHANG Hong , GUO Ying-hai , LI Zhuang-fu , ZHANG Tian-mo. Deposition and Coal Accumulation of Shanxi Formation in Kaiping-Jianhe Area[J]. Journal of China University of Mining & Technology, 2000, 29(2): 203-206
Authors:SHA Ya-nan   ZHANG Hong    GUO Ying-hai    LI Zhuang-fu    ZHANG Tian-mo
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.
Keywords:shallow water delta  coal accumulation  ingression  Shanxi Formation  Kaiping-Jianhe area
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