新疆塔里木盆地温宿凸起石油地质条件新认识

doi:10.19388/j.zgdzdc.2019.04.02

Abstract
Figure/Table
References
Related Citation (9)

Download: PDF (7049 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract In order to solve the key geological problems, such as the tectonic evolution, oil source conditions and the trap type in Wensu bulge, the authors ascertained the key factors of oil and gas accumulation and put forward the new cognitions about petroleum geology, through the comprehensive analysis of petroleum geological conditions and the results of sample test. The results show that Wensu bulge is an inherited developmental paleo-uplift, and the tectonic evolution has experienced four stages. Wensu bulge reservoir type is dominated by tectonic-lithologic types, without the development of source rocks, but it developed a high-efficiency system for communication with the hydrocarbon-rich sag in Baicheng. The reservoirs of Jidike Formation of the Neogene in Wensu bulge are dominated by tectonic-lithologic reservoirs. The hydrocarbon generation, migration and accumulation mainly occured in the Neogene-Quaternary, with obvious characteristics of late complex accumulation. The superior caprock conditions are important factors for the formation of reservoirs in Jidike Formation.

Key words： Tarim Basin Wensu bulge tectonic evolution Neogene System hydrocarbon accumulation condition

Received: 22 April 2019

ZTFLH:	P618.130.2
	TE122

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	YANG Youxing
	GAO Yongjin
	ZHANG Junfeng
	ZHOU Xingui
	ZHANG Jinhu
	MIAO Miaoqing

Cite this article:

YANG Youxing,GAO Yongjin,ZHANG Junfeng, et al. New understanding of petroleum geological conditions of Wensu bulge in Tarim Basin, Xinjiang[J]. , 2019, 6(4): 11-16.

URL:

http://www.zgdzdcbjb.com/EN/10.19388/j.zgdzdc.2019.04.02 OR http://www.zgdzdcbjb.com/EN/Y2019/V6/I4/11

[1] 贾承造,魏国齐,姚慧君,等.盆地构造演化与区域构造地质[M].北京:石油工业出版社,1995:1-70.
[2] 吕修祥,金之钧,周新源,等.塔里木盆地乌什凹陷—温宿凸起油气勘探前景[J].中国石油大学学报:自然科学版,2006,30(1):17-21,25.
[3] 席勤,余和中,顾乔元,等.塔里木盆地阿瓦提凹陷主力烃源岩探讨及油源对比[J].大庆石油地质与开发,2016,35(1):12-18.
[4] 张水昌,高志勇,李建军,等.塔里木盆地寒武系—奥陶系海相烃源岩识别与分布预测[J].石油勘探与开发,2012,39(3):285-293.
[5] 崔军文,唐哲民.塔里木盆地构造格架和构造应力场分析[J].岩石学报,2011,27(1):231-242.
[6] 何登发,白武明,孟庆任.塔里木盆地地球动力学演化与含油气系统旋回[J].地球物理学报,1998,41(增刊1):77-87.
[7] 何文渊,李江海,钱祥麟,等.塔里木盆地柯坪断隆断裂构造分析[J].中国地质,2002,29(1):37-43.
[8] 贾承造. 中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997:205-389.
[9] 张君峰,高永进,杨有星,等.塔里木盆地温宿凸起油气勘探突破及启示[J].石油勘探与开发,2019,46(1):14-24.
[10] 贾承造. 中国中西部前陆冲断带构造特征与天然气富集规律[J].石油勘探与开发,2005,32(4):9-15.
[11] 贾承造,何登发,陆洁民.中国喜马拉雅运动的期次及其动力学背景[J].石油与天然气地质,2004,25(2):121-125,169.
[12] 汤良杰,漆立新,邱海峻,等.塔里木盆地断裂构造分期差异活动及其变形机理[J].岩石学报,2012,28(8):2569-2583.
[13] 刘景彦,林畅松,赖兴运,等.塔里木盆地库车坳陷古近系库姆格列木群底砂岩段沉积古地理和物源体系[J].岩石矿物学杂志,2008,27(6):538-546.
[14] 苗继军,贾承造,戴金星,等.南天山前陆冲断带中段乌什—温宿地区构造分析与油气成藏[J].天然气地球科学,2005,16(4):428-432.
[15] 刘自亮,沈芳,朱筱敏,等.浅水三角洲研究进展与陆相湖盆实例分析[J].石油与天然气地质,2015,36(4):596-604.
[16] 邹才能,赵文智,张兴阳,等.大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布[J].地质学报,2008,82(6):813-825.
[17] 梁狄刚,陈建平,张宝民,等.塔里木盆地库车坳陷陆相油气的生成[M].北京:石油工业出版社,2004:1-60.
[18] 李谦,王飞宇,孔凡志,等.库车坳陷恰克马克组烃源岩特征[J].石油天然气学报,2007,29(6):38-42.
[19] 王飞宇,杜治利,李谦,等.塔里木盆地库车坳陷中生界油源岩有机成熟度和生烃历史[J].地球化学,2005,34(2):136-146.
[20] 龚德瑜,李明,李启明,等.塔里木盆地乌什凹陷原油地球化学特征及油源分析[J].天然气地球科学,2014,25(1):62-69.
[21] 郑民,彭更新,雷刚林,等.库车坳陷乌什凹陷构造样式及对油气的控制[J].石油勘探与开发,2008,35(4):444-451.
[22] 周延钊,鲁雪松,刘华,等.库车前陆乌什凹陷东部构造-岩性油气藏储层物性及含油性主控因素[J].天然气地球科学,2016,27(6):994-1002.
[23] 武芳芳,朱光有,张水昌,等.塔里木盆地油气输导体系及对油气成藏的控制作用[J].石油学报,2009,30(3):332-341.
[24] 戴金星,卫延召,赵靖舟.晚期成藏对大气田形成的重大作用[J].中国地质,2013,30(1):10-19.