Characteristics, main controlling factors and densification mechanisms of unconventional tight reservoirs in Triassic Yanchang Formation in southern Ordos Basin, China

被引:2
作者
Ma, Yi-Quan [1 ,2 ]
Zhang, Chen [1 ,2 ]
Lu, Yong-Chao [3 ]
Kong, Xiang-Ye [1 ]
Guo, Ying [1 ,4 ]
Dong, Yi-Xin [1 ]
Chen, Lin [5 ]
Qi, Rong [6 ]
Xing, Feng-Cun [1 ,2 ]
机构
[1] Chengdu Univ Technol, Inst Sedimentary Geol, State Key Lab Oil Gas Reservoir Geol & Exploitat, Chengdu 610059, Sichuan, Peoples R China
[2] Chengdu Univ Technol, Key Lab Deep time Geog & Environm Reconstruct, Applicat Minist Nat Resource, Chengdu 610059, Sichuan, Peoples R China
[3] China Univ Geosci Wuhan, Coll Earth Resources, Wuhan 430074, Hubei, Peoples R China
[4] Chengdu Univ Technol, Coll Management Sci, Chengdu 610059, Sichuan, Peoples R China
[5] Wuhan Ctr China Geol Survey, Wuhan 430205, Hubei, Peoples R China
[6] Sinopec North China Petr Bur Oil & Gas Co, Res Inst Petr Engn Technol, Zhengzhou 450006, Peoples R China
基金
中国国家自然科学基金;
关键词
Yanchang formation; Tight reservoirs; Densification process; Ordos basin; Reservoir evaluation; SANDSTONE RESERVOIRS; OIL-FIELD; LONGDONG AREA; QUALITY; ORIGIN; CLASSIFICATION; PERMEABILITY; POROSITY; SAND; GAS;
D O I
10.1016/j.petsci.2024.09.020
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
The key factors controlling the densification of unconventional reservoirs (e.g., tight oil and gas reservoirs) remain poorly understood and directly affect the distribution of exploitable resources. Here, systematically explored reservoir characteristics, depositional microfacies, and the main factors controlling densification of the tight oil reservoir in the Chang 8 Member (Yanchang Formation, Middle Triassic) in the southern Ordos Basin by thin section analysis, scanning electron microscopy, physical property measurement, X-ray diffraction, and mercury injection. Our results confirm the Chang 8 reservoir as an extremely low permeability tight sandstone reservoir mainly comprising lithic feldspathic sandstone with various primary and secondary pores and fine pore channels. The highest quality reservoir is mainly restricted to the middle and lower parts of subaqueous distributary channel microfacies. Dissolution partly contributed to reservoir formation, but the persistence of early, non-compressed storage space was more important. The compression of plastic rock debris removed a significant amount of porosity, and calcite, kaolinite, and siliceous minerals both fill pores, whereas chlorite cladding of particles protects the pore space. We identified three densification mechanisms: the persistent densification of highly plastic rock debris during burial, calcite cementation and pore filling, and feldspar dissolution and subsequent kaolinite precipitation and siliceous cementation. After their compaction, the Chang 8 Member reservoirs were charged with hydrocarbons. We applied clustering analysis to eight reservoir characteristics (porosity, permeability, median pore-throat radius, maximum pore-throat radius, median capillary pressure, pore discharge pressure, chlorite content, kaolinite content) to quantitatively classify the Chang 8 reservoir into three categories. Type-I reservoirs have the best conditions for hosting tight oil reservoirs, with similar to 12% porosity, permeabilities of similar to 0.2 x 10(-3) mu m(2), trial oil production rates of >5 m(3)/d, and, indeed, occur in subaqueous distributary channel microfacies. Type-II reservoirs similar to 10% porosity, permeabilities of similar to 0.1 x 10(-3) mu m(2), and trial oil production rates of 1-5 m(3)/d. Type-III reservoirs have similar to 5% porosity, permeabilities of similar to 0.05 x 10(-3) mu m(2), and trial oil production rates <1 m(3)/d. These results provide an important basis for predicting the distribution of exploitable zones in the Chang 8 Member and other adjacent tight reservoirs. (c) 2024 The Authors. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/ 4.0/).
引用
收藏
页码:3884 / 3898
页数:15
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