油气地质

鄂尔多斯盆地西北部上三叠统延长组复合油藏成藏机理

  • 赵 岩 ,
  • 贺振华 ,
  • 黄德济
展开
  • 1.中国石油长庆油田勘探开发研究院;2.陕西西安低渗透油气田勘探开发国家工程实验室; 3.中国石油东方地球物理公司东部事业勘探部长庆经理部;4.中国石油长庆油田油藏评价处
李元昊,1976 年生,男,博士,工程师,从事石油地质综合研究工作。地址:(710018)陕西省西安长庆油田兴隆园小区勘探开发研究院。电话:(029)86598494。E-mail: liyuanh_cq@petrochina.com.cn

网络出版日期: 2010-06-15

基金资助

鄂尔多斯盆地大型岩性地层油气藏勘探开发示范工程(编号:2008ZX05044)项目资助

Accumulation mechanism of composite reservoir of Upper Triassic Yanchang Formation in northwestern Ordos Basin

  • ZHAO Yan ,
  • HE Zhenhua ,
  • HUANG Deji
Expand
  • (1.ResearchInstitute ofExploration andDevelopment,ChangqingOi~ ldCompany,PetroChina,Xi’all 710018,China; 2.State Engineering Laboratory ofLow Permeability Oil and Gas Field Exploration and Development,Xi’an 7 1001 8,China; 3.ChangqingExploration Department,Bureau ofGeophysical Prospecting,China National Petroleum Corporation, Xi’an 710018,China;4 Reservoir Description Department,Changqing Oitfield Company,PetroChina,Xi’an 710018,China

Online published: 2010-06-15

摘要

鄂尔多斯盆地西北部上三叠统延长组主要发育湖泊一三角洲沉积,是近年来石油重点勘探层系之一。长7段油页岩为烃源岩,生烃增压作用是长7段烃源岩异常高压形成的主要机制,异常高压是石油运移的主要动力。原油通过流体压裂缝、断层和叠置砂体进行运移,压力越大越有利于低渗透储层成藏。长7段烃源岩具有连续式生烃、幕式排烃、多点式充注成藏特征。包裹体均一温度、成岩特征等表明.烃源岩先向下再向上排烃,二次运移具有垂向运移为主、短距离侧向运移特征。利用声波时差测井曲线计算了长7段向下排烃厚度平均约10 in,向上排烃厚度平均约30 ITI,向下与向上排烃量之比约为l:3。

本文引用格式

赵 岩 , 贺振华 , 黄德济 . 鄂尔多斯盆地西北部上三叠统延长组复合油藏成藏机理[J]. 岩性油气藏, 2010 , 22(2) : 32 -36 . DOI: 10.3969/j.issn.1673-8926.2010.02.006

Abstract

The Yanehang Formation in northwestern Ordos Basin is one of the most important exploration area which mainly developed lacustrine delta deposition.The Chang 7 oil shale is the source rock which produced high pressure during the main period of hydrocarbon generation.The overpressure is the main dynamic force for the oil migration to the low perm eability reservoirs through microfraetures faults and superposed sands.The Chang 7 sourae rock is characterized by continuous hydrocarbon-generation,episodic hydrocarbon expulsion and muhipoint injection.The source rocks firstly expeHed down to the lower reservoirs and then to the upper reservoirs according to the homogenization temperature and diagenesis and the secondary migration is mainly vertical and short lateral migration.The thickness of downward expulsion is 10 meter and the upper is 30 meter.The ratio of the upper and down hydrocarbon expulsion amount ofchang 7 is about 3:1.

参考文献

[1] 宋凯,吕剑文,凌升阶,等.鄂尔多斯定边—吴旗地区前侏罗纪古地貌与油藏[J].古地理学报,2003,5(4):497-505.
[2] 刘华清,袁剑英,李相博,等.鄂尔多斯盆地延长期湖盆演化及其成因分析[J].岩性油气藏,2007,19(1):52-56.
[3] 张文正,杨华,傅锁堂,等.鄂尔多斯盆地长91 湖相优质烃源岩的发育机制探讨[J].中国科学(D)地球科学,2007,37(增刊):33-38.
[4] 邱楠生,胡圣标,何丽娟,等. 沉积盆地热体制研究的理论与应用[M].北京:石油工业出版社,2004:15-21.
[5] 田在艺,张庆春.中国含油气沉积盆地论[M].北京:石油工业出版社,1996:114-130.
[6] 李明诚,单秀琴,马成华,等.油气成藏期探讨[J].新疆石油地质,2005,26(5):587-590.
[7] 李元昊,刘池洋,王秀娟,等.鄂尔多斯盆地西北部延长组下部幕式成藏特征[J].石油学报,2009,30(1):61-66.
[8] 张文正,杨华,李剑锋,等.论鄂尔多斯盆地长7 段段优质油源岩在低渗透油气成藏富集中的主导作用———强生排烃特征及机理分析[J].石油勘探与开发,2006,33(3):289-293.
[9] 付广,李晓伟.源外上生下储成藏主控因素及有利区预测———以松辽盆地尚家地区泉二段为例[J].岩性油气藏,2009,21(1):1-5.
[10] 郑荣才,胡诚,董霞.辽西凹陷古潜山内幕结构与成藏条件分析[J]. 岩性油气藏,2009,21(4):10-18.
[11] 冯莉恒. 基于声波时差的超压源岩上、下排烃分配量方法及其应用[J].大庆石油学院学报,2007,31(1):22-24,37.
[12] 姚泾利,王克,宋江海,等. 鄂尔多斯盆地姬塬地区延长组石油运聚规律研究[J].岩性油气藏,2007,19(3):32-37.
文章导航

/