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二连盆地霍林河地区低煤阶煤层气成藏条件及主控因素
引用本文:雷怀玉,孙钦平,孙斌,李五忠,陈刚,田文广.二连盆地霍林河地区低煤阶煤层气成藏条件及主控因素[J].天然气工业,2010,30(6):26-30.
作者姓名:雷怀玉  孙钦平  孙斌  李五忠  陈刚  田文广
作者单位:1.北京大学工学院;2.中国石油勘探与生产公司;3.中国石油勘探开发研究院廊坊分院
摘    要:我国越来越重视对低煤阶煤层气的勘探,但已有的资料表明,目前对低煤阶煤层气藏的认识还不够深入。为此,以我国典型的低煤阶煤层气区——二连盆地霍林河地区为例,对该区煤层气地质特征和煤岩煤质及煤岩演化程度、煤储层渗透性、煤层含气性等煤储层特征进行了分析,从构造条件、封盖条件及水文地质条件3个方面研究了煤层气藏主控因素及保存条件。结论认为:霍林河地区煤层气成藏条件有利,具有煤层厚度大、煤层埋深较浅、煤储层渗透性好、含气量较高、封闭保存条件好等特点;保存条件是该区煤层气成藏的主控因素,且封闭条件好的浅部是煤层气富集的有利区。

关 键 词:二连盆地  霍林河地区  低煤阶  煤层气  成藏条件  主控因素  储层特征  盖层封闭

Conditions and major controlling factors of coalbed methane accumulation in coal reservoirs with low coal rank in the Huolinhe area, Erlian Basin
Lei Huaiyu , Sun Qinping , Sun Bin , Li Wuzhong , Chen Gang , Tian Wenguang.Conditions and major controlling factors of coalbed methane accumulation in coal reservoirs with low coal rank in the Huolinhe area, Erlian Basin[J].Natural Gas Industry,2010,30(6):26-30.
Authors:Lei Huaiyu  Sun Qinping  Sun Bin  Li Wuzhong  Chen Gang  Tian Wenguang
Affiliation:1.College of Engineering, Peking University, Beijing 100871, China; 2.Exploration & Production Company, PetroChina, Beijing 100011, China; 3.Langfang Branch, Petroleum Exploration & Development Research Institute, PetroChina, Langfang, Hebei 065007, China
Abstract:Exploration of CBM in coal reservoirs with low coal rank has been drawing more and more attentions in China. However, current available data show that the CBM reservoirs with low coal rank are still poorly understood. By taking the Huolinhe area in the Erlian Basin, a typical Chinese CBM gas zone with low coal rank, as an example, we analyzed the CBM geological features, quality and thermal maturity of coals as well as permeability and gas potential of coal reservoirs. The major controlling factors and preservation conditions of CBM reservoirs are studied in respect of structural, sealing, hydrogeologic conditions. The coal reservoirs in the Huolinhe area are featured by large thickness, shallow burial depth, high permeability, high gas content, good seals, thus are favorable for CBM accumulation. Sealing is the major factor controlling CBM accumulation in the study area, and favorable CBM plays exist in shallow layers with good seals.
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