CHARACTERISTICS AND ESTIMATE OF CARBONIFEROUS SOURCE ROCKS IN BAYEHOT BASIN
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摘要: 以地表和井下烃源岩样品分析数据为依据,阐述巴彦浩特盆地石炭系烃源岩的分布、地化特征及影响因素,并进行综合评价。研究结果表明,巴彦浩特盆地发育暗色泥岩、灰岩2种源岩,分布于中、下石炭统臭牛沟组、靖远组和羊虎沟组。暗色泥岩有机质丰度中等—好,以腐泥—腐殖型和腐殖型为主,普遍进入成熟—高成熟阶段,是好的烃源岩。碳酸盐岩有机质丰度较低,具有一定的生烃能力,但厚度较小,分布局限,生烃潜力不大。沉积环境和构造运动对有机质丰度和热演化程度影响较大。巴彦浩特盆地有利生油区分布于乌达—巴参2—锡1井—查汗布勒格以北的北东向展布的滨浅海三角洲及近岸浅海环境沉积区。Abstract: According to analyses data of source rock samples from surface and underground,it is described in this paper distribution,geochemical characteristics and influential factors of Carboniferous source rocks in the Bayehot Basin.2 types of source rocks are generated in the basin: dark mudstone and limestone,mainly locating in the Chouniugou,Jingyuan and Yanghugou Formations of the Middle-Lower Carboniferous.Dark mudstone works as good source rock,with middle-good organic abundance,sapropel-humic and humic organic types as well as mature-high mature generation stage.Carbonate with lower organic abundance can generate certain hydrocarbon,yet has poor generation potential with less thickness and limited distribution.Sedimentary environment and tectonic movement have great influence on abundance and thermal evolution extent of organic matters.The most favorable source area of Bayehot Basin distribute in the sedimentary area of littoral-neritic delta and near-shore shallow sea facies trending NE to the north of Wuda-Bacan2-Xi1-Chahabuleg.
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Key words:
- organic abundance /
- organic maturity /
- source rock /
- Carboniferous /
- Bayehot Basin
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[1] 刘绍平,刘学锋.巴彦浩特盆地的构造类型[J].西南石油学院学报,2002,24(3):24-27 [2] 熊保贤,陈文学,陈文礼等.巴彦浩特原型盆地形成与演化[J].石油实验地质,2001,23(1):19-22 [3] 张明洁,杨品.准噶尔盆地石炭系(油)气藏特征及成藏条件分析[J].新疆石油学院学报,2000,12(6):8-13 [4] 张朝军,石昕,吴晓智等.准噶尔盆地石炭系油气富集条件及有利勘探领域预测[J].中国石油勘探,2005,10(1):11-16 [5] 卫平生,李天顺,李安春等.巴彦浩特盆地石炭系沉积相及沉积演化[J].沉积学报,2005,23(2):240-246 [6] 曹代勇,刘善印,张守仁等.河西走廊-巴彦浩特盆地石炭系含油气远景评价[J].西北地质,2003,36(1):62-69 [7] 熊保贤,孙自明,肖波等.巴彦浩特盆地石炭系含油气系统及有利区带分析[J].现代地质,2000,14(4):429-434 [8] 王寿清.对巴彦浩特盆地油气勘探的意见[J].河南石油,2000,(6):1-7 [9] 宋桂桥,马玉春,刘传川等.巴彦浩特盆地构样式分析及其意义[J].河南石油,1999,(4):8-14 [10] 孙东胜,白玉宝,蔚远江.祁连-走廊-贺兰坳陷区石炭系油气勘探有利区块选择[J].石油与天然气地质,2000,21(1):84-87 [11] 刘学锋.巴彦浩特盆地构造特征及含油气远景初步评价[J].西南石油学院学报,1994,16(4):18-27 [12] 张世晖,刘天佑,顾汉明等.巴彦浩特盆地火成岩的综合地球物理解释[J].物探与化探,2003,27(5):383-386
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