The forming mechanism and process of tight oil sand reservoirs: A case study of Chang 8 oil layers of the Upper Triassic Yanchang Formation in the western Jiyuan area of the Ordos Basin, China

被引:45
作者
Wang, Yang [1 ,2 ]
Liu, Luofu [1 ,2 ]
Li, Shutong [3 ]
Ji, Haitao [1 ,2 ]
Xu, Zhengjian [1 ,2 ]
Luo, Zehua [1 ,2 ]
Xu, Tong [1 ,2 ]
Li, Linze [1 ,2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Engn, Beijing 102249, Peoples R China
[2] China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China
[3] Chinese Acad Sci, Inst Geol & Geophys, Gansu Prov Key Lab Petr Resources Res, Key Lab Petr Resources, Lanzhou 730000, Gansu, Peoples R China
基金
高等学校博士学科点专项科研基金; 中国国家自然科学基金;
关键词
Tightening process; Tightening mechanism; Diagenesis; Chang 8 oil layer; Western Jiyuan area; Ordos Basin; LOW PERMEABILITY RESERVOIR; SECONDARY POROSITY; CARBONATE CEMENTS; LONGDONG AREA; SANDSTONES; DIAGENESIS; QUALITY; GAS; ACCUMULATION; COMPACTION;
D O I
10.1016/j.petrol.2017.08.026
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Upper Triassic Yanchang Formation in the Ordos Basin, northwest China, comprise the typical tight oil reservoirs, which have porosity less than 10% and permeability less than 1 mD. The western Jiyuan area (WJA), at the western margin of th e Ordos Basin, has made significant progress in the tight oil exploration of the Yanchang Formation recently. Whereas the lack of recognition of tightening mechanism and process of reservoirs resulting in the misunderstanding of tight oil reservoirs prediction. This study focuses on the petrology, diagenetic processes, as well as forming mechanism and process of the Chang 8 (Ch-8) tight oil reservoirs located in the WJA. Four conclusions were reached. First, Ch-8 tight reservoirs, which are mainly composed of lithic arkose and feldspathic litharenite, experienced diagenesis, such as mechanical and chemical compaction, cementation, and dissolution. The reservoirs are at the late period of the mesogenetic A stage. Second, the tightness of the Ch-8 reservoirs is due to both sedimentary and diagenetic factors. The sedimentary environment where sand bodies are close to the provenance that has a rapidly increasing lacustrine level provides conditions for reservoir tightness. The initial porosity rapidly decreases due to compaction and cementation which produce porosity loss rates of 49.42% and 40.87%, respectively. By contrast, the effect of dissolution is limited, as it only increases porosity by 4.48%. Third, the tightening process of the Ch-8 reservoirs comprise four stages: compaction causes pores to reduce rapidly; followed by early cementation, which causes pores to reduce; dissolution, which causes pores to increase slightly; and late cementation, which causes tightness. Finally, it is likely that the Ch-8 reservoirs were already tight prior to hydrocarbon accumulation, thus demonstrating that they represent typical tight oil reservoirs.
引用
收藏
页码:29 / 46
页数:18
相关论文
共 80 条
[1]  
[Anonymous], EFLCIENCY
[2]  
BEARD DC, 1973, AM ASSOC PETR GEOL B, V57, P349
[3]  
BJORLYKKE K, 1989, GEOL RUNDSCH, V78, P243
[4]   Relationships between depositional environments, burial history and rock properties. Some principal aspects of diagenetic process in sedimentary basins [J].
Bjorlykke, Knut .
SEDIMENTARY GEOLOGY, 2014, 301 :1-14
[5]  
[陈瑞银 Chen Ruiyin], 2006, [石油学报, Acta Petrolei Sinica], V27, P43
[6]  
[陈修 Chen Xiu], 2016, [沉积学报, Acta Sedimentologica Sinica], V34, P364
[7]   Tight gas in China and its significance in exploration and exploitation [J].
Dai Jinxing ;
Ni Yunyan ;
Wu Xiaoqi .
PETROLEUM EXPLORATION AND DEVELOPMENT, 2012, 39 (03) :277-284
[8]  
[邓秀芹 Deng Xiuqin], 2009, [石油与天然气地质, Oil & Gas Geology], V30, P156
[9]  
[丁晓琪 Ding Xiaoqi], 2007, [石油与天然气地质, Oil & Gas Geology], V28, P491
[10]  
DIXON SA, 1985, AAPG BULL, V69, P250