[1]朱春俊,王延斌.鄂尔多斯盆地东北部上古生界煤系地层成煤特征分析[J].西安科技大学学报,2010,(06):687-692730.
 ZHU Chun-jun,WANG Yan-bin.Characteristic analysis of coal forming in the coal-bearing formation of Paleozoic in the northeast of Ordos basin[J].Journal of Xi’an University of Science and Technology,2010,(06):687-692730.
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鄂尔多斯盆地东北部上古生界煤系地层成煤特征分析()
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西安科技大学学报[ISSN:1672-9315/CN:61-1434/N]

卷:
期数:
2010年06期
页码:
687-692730
栏目:
出版日期:
2010-11-11

文章信息/Info

Title:
Characteristic analysis of coal forming in the coal-bearing formation of Paleozoic in the northeast of Ordos basin
文章编号:
1672-9315(2010)06-0687-05
作者:
朱春俊王延斌
中国矿业大学(北京)研究生院,北京 100083
Author(s):
ZHU Chun-junWANG Yan-bin
Faculty of Graduate Students,China University of Mining and Technology(Beijing),Beijing 100083,China
关键词:
鄂尔多斯盆地 上古生界 成煤特征 聚煤控制因素
Keywords:
ordos basin paleozoic erathem coal forming characteristics controlling factor of coal accumulation
分类号:
TD163+.1
文献标志码:
A
摘要:
依据基准面旋回的原理,应用露头、钻(测)井资料,研究了鄂尔多斯盆地东北部上古生界煤层的空间变化和平面分布规律。结果表明:受古地形和古气候的影响,在构造转换间歇期的不同沉积环境中,受基准面旋回和相分异作用控制,研究区煤层多形成于短期基准面上升的晚期,并以障壁海岸沉积的煤层分布广,厚度大;三角洲沉积体系中,煤层多发育在三角洲平原沼泽中;而辫状河道沉积体系中,受河道对下伏地层的冲刷迁移影响,煤层则出现分叉、变薄或尖灭,多不能形成规模煤层。
Abstract:
基于基准面循环原理,利用露头和钻井研究了鄂尔多斯盆地东北部古生界煤层煤层的空间变异和表面分布规律。 结果表明,受古地貌和古气候的影响,在基准面旋回和相分异作用下,煤层在转变休眠期不同矿床环境中的短期基准面周期后期形成。煤层在屏障岛上分布广泛,厚度大,在三角洲沉积体系中,煤分布在三角洲平原的泥潭中。 在辫状河道沉积系统中,受河道冲刷和河道向下层迁移的影响,煤层似乎分叉,

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备注/Memo

备注/Memo:
收稿日期:2010-06-17基金项目:国家自然科学基金项目(40272070)通讯作者:朱春俊(1977-),男,山西洪洞人,博士研究生,工程师,主要从事煤炭地质领域的研究工作。
更新日期/Last Update: 2010-11-11