›› 2013, Vol. 34 ›› Issue (5): 1-1.

• 论文 •    

中国近海新生代含油气盆地成煤特征

张海涛,朱炎铭   

  1. (中国矿业大学 a.资源与地球科学学院;b.煤层气资源与成藏过程教育部重点实验室,江苏 徐州 221116)
  • 出版日期:2019-01-01 发布日期:1905-07-13

CoalForming Characteristics of Cenozoic Petroliferous Basins in Offshore China

ZHANG Haitaoa,b, ZHU Yanminga,b   

  1. (China University of Mining and Technology, a.School of Resources and Earth Science, b.MOE Key Lab of Coal Bed Methane and Deposit Process, Xuzhou, Jiangsu 221116, China)
  • Online:2019-01-01 Published:1905-07-13

摘要: 对中国近海含油气盆地特征进行了探讨,讨论了构造、气候、沉积及物源特征,对比渤海湾盆地、南黄海盆地、东海陆架盆地、珠江口盆地、琼东南盆地、北部湾盆地及莺歌海盆地含煤地层发育情况,揭示中国近海盆地新生代煤层分布特征:中国近海盆地有3次成煤期,成煤环境一般,煤层层数多、厚度薄、煤阶低、展布局限;由北向南,由西向东,成煤时代逐渐变新,主要成煤期与构造事件、气候事件相一致。

Abstract: Starting from the basic factors affecting coal forming, this paper discusses the features of tectonic, climate, sediment and provenance, correlates the coal?bearing strata in Bohai Bay basin, South Yellow Sea basin, East China Sea shelf basin, the Pearl River Mouth basin, Qiongdongnan basin, Beibu Gulf basin and Yinggehai basin, and reveals the Cenozoic coal seam distribution characteristics in these China’s offshore basins. The results show that there are three coal?forming stages in these basins, with general environment for coal forming, numerous coal layer, thin thickness, low coal rank and local extension, and the coal?forming eras gradually become newer from north to south and from west to east, the main coal?forming stages are consistent with the tectonic events and the climate events

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