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惠民凹陷南坡煤型气有效供气中心分析
引用本文:陈庆春,陈永红,王秀鹏.惠民凹陷南坡煤型气有效供气中心分析[J].高校地质学报,2002,8(4):429-436.
作者姓名:陈庆春  陈永红  王秀鹏
作者单位:1. 南京大学地球科学系,南京 210093 ; 2. 胜利石油管理局临盘采油厂,山东东营251507
摘    要:惠民凹陷南坡石炭-二叠系煤层分布广泛,厚度较大,为一套以潮坪-泻湖沉积为主的海陆交互相地层,其有机质属浅沼森林有机相和深沼芦苇有机相。生气模拟实验表明,太原组和山西组煤岩生气潜力分别达150mL/g有机碳和110mL/g有机碳,煤型气源岩经历了复杂的热演化过程,其有效二次生气时期为早第三纪至今,门限温度135℃,对应的埋深入4000m,有效供气中心位于济阳地堑东部和曲堤地垒东段, 生气强度一般达到(20-40)×10^8m^3/km^2。位于主导运聚方向上的曲堤地垒东段是今后勘探的重点目标。

关 键 词:惠民凹陷  煤型气  模拟实验  二次生气  煤型气源岩  渤海湾盆地
文章编号:1006-7493(2002)04-429-08
收稿时间:2002-12-20
修稿时间:2002年1月3日

Analysis of Effective Generation Center of Coal-Formed Gas in South Slope of Huimin Sag
CHEN Qing chun ,CHEN Yong hong ,WANG Xiu peng.Analysis of Effective Generation Center of Coal-Formed Gas in South Slope of Huimin Sag[J].Geological Journal of China Universities,2002,8(4):429-436.
Authors:CHEN Qing chun    CHEN Yong hong  WANG Xiu peng
Institution:1. Department of Earth Sciences, Nanjing University, Nanjing 210093, China; 2. Linpan Oil Development Factory of Shenli Oilfield, Dongying, Shandong 251507, China
Abstract:Coal beds occur in a wide area and developed with big thickness in south slope of Huimin Sag.These coal beds are sediments of marine-terrestrial interface which deposited under environments of tidal flat and lagoon.It is shown by gas generation simulation experiments that the gas generation potential of the Taiyuan and Shanxi Formation are 150mL/g and 1 10mL/g organic matter respectively.The source rock of coal-formed gas has a very complex thermal evolution process.The second gas generation occurred from the Early Tertiary to the Quaternary, with a threshold tempreture of 135℃ and corresponding depth of 4000m..The effective gas generation center is located in eastern of the Jiyang Graben and Quti Horst.The gas generation intensity is about 20 ×10 8m3/km2 to 40 ×10 8m3/km. Therefore,eastern parts of Quti Horst is the main target of exploration.
Keywords:south slope of Huimin Sag  coal  formed gas  simulation experiment  gas generation at second evolution stage  effective gas generation center
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