«Previous Article|Table of Contents|Next Article»

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:

2011年第04期

Page:

364-372

Research Field:

基础地质与矿产地质

Publishing date:

Info

Title:

Review on Oil/gas Accumulation with Low Permeability in Ordos Basin

Author(s):

LI Rong-xi¹; 2; DUAN Li-zhi¹; 2; ZHANG Shao-ni¹; 2; CHEN Bao-yun¹; 2; SHI Bin³; YAN Gai-ping⁴

1. School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Key Laboratory of West Mineral Resources and Geological Engineering of Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Institute

Keywords:

low permeable reservoir;  primary migration;  secondary migration;  accumulation;  lithological reservoir;  Ordos Basin

PACS:

TE122.1;P618.130.1

DOI:

-

Abstract:

Ordos Basin is the largest base for low permeable oil/gas exploration and development in China. The low permeable oil/gas accumulation in Ordos Basin featured with poor physical property, strong heterogeneity and complex factors controlling oil/gas accumulation and distribution. Based on reviewing and summarizing the history and experience of low permeability reservoir exploration in Ordos Basin, it indicated that there are two theory systems in studying low permeability reservoir formation at present. One is sedimentary controlling reservoir formation theory, which emphasizes that low permeability reservoir formation was controlled by sedimentary facies, heterogeneity and diagenesis; the other one is dynamics controlling reservoir formation theory, which focuses on oil/gas migration dynamics in primary migration and secondary migration. At present, it is insufficient to study low permeable oil/gas accumulation because traditional theories emphasize on single factor controlling oil/gas accumulation and corresponding exploration, which can not exactly reveal oil/gas accumulation principle and effectively guide exploration. Similarities and differences between low permeability reservoirs and conventional reservoirs should be paid attention. The sedimentary controlling reservoir formation theory limited to divide sedimentary facies and to establish depositional model; it emphasized on the controls of sedimentary factors to oil/gas accumulation, and ignored the dynamic properties of hydrocarbon accumulation process. Dynamics controlling reservoir formation theory overemphasizes the modeled and formulistic oil/gas fluid migration; it exaggerated and optionally explained the role of oil/gas migration and accumulation record(oil/gas inclusion)and its original geological significance, and ignored the complex of oil/gas migration and the multiplicity of oil/gas inclusion record. It is important to study reservoir geological record and reservoir formation history to summarize oil/gas accumulation principle and to provide important data for oil and gas exploration.

References:

[1] 李道品,张连春.我国低渗透油田开发当前之新进展[J].低渗透油气田,2004,9(1):1-9.
[2] 付金华,魏新善,任军峰,等.鄂尔多斯盆地天然气勘探形势与发展前景[J].石油学报,2006,27(6):1-4.
[3] 李德生.重新认识鄂尔多斯盆地油气地质学[J].石油勘探与开发,2004,31(6):1-7.
[4] 马新华.鄂尔多斯盆地天然气勘探开发形势分析[J].石油勘探与开发,2005,32(4):50-53.
[5] 王道富,杨 华,付金华.鄂尔多斯盆地天然气勘探开发战略研讨[J].天然气工业,2005,25(4):1-4.
[6] 杨 华,付金华,魏新善.鄂尔多斯盆地天然气成藏特征[J].天然气工业,2005,25(4):5-8.
[7] 张厚福,王永诗.油气藏研究的历史、现状与未来[M].北京:石油工业出版社,2007.
[8] 张厚福,徐兆辉.从油气藏研究的历史论地层-岩性油气藏勘探[J].岩性油气藏,2008,20(1):114-123.
[9] Pan C H.Nonmarine Origin of Petroleum in North Shensi, and the Cretaceous of Szechuan, China[J].AAPG Bulletin,1941:25(11):2058-2068.
[10] 杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002.
[11] 朱国华.陕北浊沸石次生孔隙砂体的形成与油气关系[J].石油学报,1985,6(1):1-8.
[12] 朱国华.碎屑岩储集层孔隙的形成、演化和预测[J].沉积学报,1992,10(3):114-123.
[13] 席胜利,刘新社,王 涛.鄂尔多斯盆地中生界石油运移特征分析[J].石油实验地质,2004,26(3):229-235.
[14] 罗晓容,喻 建,张发强,等.二次运移数学模型及其在鄂尔多斯盆地陇东地区长8段石油运移研究中的应用[J].中国科学:D辑,2007,37(增):73-82.
[15] 李道品,罗迪强,刘雨芬.低渗透油田概念及我国储量分布状况[J].低渗透油气田,1996,1(1):1-8.
[16] 蒋凌志,顾家裕,郭彬程.中国含油气盆地碎屑岩低渗透储层的特征及形成机理[J].沉积学报,2004,22(1):13-18.
[17] 汤锡元,陈荷立.陕甘宁盆地西缘逆冲推覆构造及油气勘探[M].西安:西北大学出版社,1992.
[18] 赵重远.鄂尔多斯及山西地块地质构造及沉积盆地的形成、演化及其与油气关系[M].北京:石油工业出版社,1988.
[19] 刘池洋,赵红格,王 锋,等.鄂尔多斯盆地西缘(部)中生代构造属性[J].地质学报,2005,79(6):737-747.
[20] 张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油实验地质,2004,26(2):138-142.
[21] Liu S F.The Coupling Mechanism of Basin and Orogen in the Western Ordos Basin and Adjacent Regions of China[J].Journal of Asian Earth Sciences,1998,16(4):369-383.
[22] 邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003,24(2):34-37.
[23] 贾承造,魏国齐,李本亮.中国中西部燕山期构造特征及其油气地质意义[J].石油与天然气地质,2005,26(1):9-15.
[24] 王庭斌.中国气藏主要形成、定型于新近纪以来的构造运动[J].石油与天然气地质,2004,25(2):126-132.
[25] 马文杰,陈丽华,王雪松.我国致密碎屑岩天然气储层特征[J].低渗透油气田,1997,2(4):8-13.
[26] 李文厚,魏红红,马振芳,等.苏里格庙气田碎屑岩储集层特征与天然气富集规律[J].石油与天然气地质,2002,23(4):387-391.
[27] 史基安,王金鹏,毛明陆,等.鄂尔多斯盆地西峰油田三叠系延长组长6—8段储层砂岩成岩作用研究[J].沉积学报,2003,21(3):373-380.
[28] 禚喜准,王 琪,史基安.鄂尔多斯盆地盐池—姬塬地区三叠系长2砂岩成岩演化特征与优质储层分布[J].矿物岩石,2005,25(4):98-106.
[29] 刘 勇,金晓辉,雷天成.鄂尔多斯盆地延长组油气初次运移特征[J].西安石油学院学报,1997,12(1):8-11.
[30] 罗静兰,刘小洪,林 潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报,2006,80(5):664-673.
[31] 席胜利,刘新社.鄂尔多斯盆地中生界石油二次运移通道研究[J].西北大学学报:自然科学版,2005,35(5):628-632.
[32] 李荣西,席胜利,邸领军.用储层油气包裹体岩相学确定油气成藏期次——以鄂尔多斯盆地陇东油田为例[J].石油与天然气地质,2006,27(2):194-199.
[33] 陈荷立.油气运移研究的有效途径[J].石油与天然气地质,1995,16(2):126-131.
[34] Hanson A D,Ritts B D,Moldowan J W.Organic Geochemistry of Oil and Source Rock Strata of the Ordos Basin,North-central China[J].AAPG Bulletin,2007,91(9):1273-1293.
[35] Yang Y T,Li W, Ma L.Tectonic and Stratigraphic Controls of Hydrocarbon Systems in the Ordos Basin:a Multicycle Cratonic Basin in Central China[J].AAPG Bulletin,2005,89(2):255-269.
[36] 张文正,杨 华,李剑锋,等.论鄂尔多斯盆地长7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.
[37] 刘林玉,王震亮,高 潮.真实砂岩微观模型在鄂尔多斯盆地泾川地区长8砂岩微观非均质性研究中的应用[J].地学前缘,2008,15(1):80-84.
[38] 杨 华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用:地质地球化学特征[J].地球化学,2005,34(2):147-154.
[39] Hindle A D. Petroleum Migration Pathways and Charge Concentration: a Three-dimensional Model[J]. AAPG Bulletin, 1997, 81(9):1451-1481.
[40] 王 琪,禚喜准,陈国俊,等.鄂尔多斯西部长6砂岩成岩演化与优质储层[J].石油学报,2005,26(5):17-23.
[41] 王彩萍.鄂尔多斯盆地直罗油田长6油层组成岩作用及孔隙演化研究[J].地球科学与环境学报,2010,32(2):161-165.
[42] 石 彬.鄂尔多斯盆地姬塬地区延长组油气成藏特征研究[D].西安:长安大学,2008.

Memo

Memo:

-

Common functions

Last Update: 2011-12-20