Characteristics and hydrocarbon-generating potential of Carboniferous source rock in Tacheng Basin
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摘要: 在塔城盆地野外露头和塔参1井钻井烃源岩发育特征与有机地化特征分析的基础上,探讨了石炭系烃源岩的生烃潜力。通过烃源岩岩性与有机质丰度分析认为,较好的烃源岩主要为泥质岩,其次为碳质泥岩和煤,上石炭统泥岩总体要好于下石炭统。烃源岩母质类型主要为腐殖型,具有倾气型特征。烃源岩演化程度普遍达到了高—过成熟阶段,但仍有一定的残余生烃潜力。应加强烃源岩主要分布区及其生烃史与盆地构造演化的匹配关系和成藏历史的研究。Abstract: Based on the analyses of generation and organic geochemical characteristics of outcrops in the Tacheng Basin and source rocks from well Tacan 1,the hydrocarbon-generating potential of the Carboniferous source rocks was discussed.According to the lithology and organic abundance of source rocks,mudstones were good source rocks while carbonaceous mudstones and coals were also favorable.The mudstones in the Upper Carboniferous were generally more favorable than those in the Lower Carboniferous.The organic material types of source rocks were mainly humus ones with gas-generating feature.Source rock evolution had entered the high-mature and over-mature stages,but there still existed residual hydrocarbon-generating capacity.Studies should be focused on the main distribution areas of source rocks,the relationship between hydrocarbon generation and basin evolutions histories,and the history of accumulation.
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[1] 阿依努尔·孜牙别克.新疆塔城地区河流水文特征[J].水文,2003,23(1):54-56. [2] 冯乾文,郑光华,张晓帆,等.塔城盆地石炭系基底的重磁电震联合反演[J].新疆大学学报,2009,26(2):242-246. [3] 张朝军,何登发,吴晓智,等.准噶尔多旋回叠合盆地的形成与演化[J].中国石油勘探,2006,1(1):47-58. [4] 况军.地体拼贴与准噶尔盆地的形成演化[J].新疆石油地质,1993,14(2):126-132. [5] 蔡忠贤,陈发景,贾振远.准噶尔盆地的类型和构造演化[J].地学前缘,2000,7(4):12-16. [6] 谷艳玲,方相阳,韩学富,等.塔城盆地古生界烃源岩评价[J].科技资讯,2011(28):1-2. [7] 李德江,杨俊生,朱筱敏.准噶尔盆地层序地层学研究[J].西安石油大学学报(自然科学版),2005,20(3):60-70. [8] 谢庆宾,管守锐,韩军,等.准东白家海—五彩湾地区层序地层特征[J].新疆石油地质,2003,24(1):31-34. [9] 潘春孚,纪友亮,高志勇,等.准噶尔盆地南缘新近系层序类型与发育模式研究[J].断块油气田,2011,18(1):34-37. [10] 李志明,关德范,徐旭辉,等.有效泥质油源岩有机碳丰度评价标准研究:以东营凹陷为例[J].石油实验地质,2009,31 (4):379-383. [11] 赵政璋,李永铁,叶和飞,等.青藏高原海相烃源层的油气生成[M].北京:科学出版社,2000. -
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