Pore structure and oil-bearing property of laminated and massive shale of Lucaogou Formation in Malang Sag, Santanghu Basin

被引:3
作者
Guo, Xiaobo [1 ,2 ,7 ]
Zhou, Longfei [1 ,2 ]
Pan, Yongshuai [3 ,8 ]
Huang, Zhilong [3 ]
Chen, Xuan [4 ]
Mu, Shangchao [5 ]
Zhang, Chenglin [6 ]
Wang, Shaoxia [4 ]
机构
[1] Xian Shiyou Univ, Sch Earth Sci & Engn, Xian, Peoples R China
[2] Xian Shiyou Univ, Shaanxi Key Lab Petr Accumulat Geol, Xian, Peoples R China
[3] Northeast Petr Univ, Key Lab Continental Shale Hydrocarbon Accumulat &, Minist Educ, Daqing, Peoples R China
[4] Tuha Oilfield Co, Res Inst Explorat & Dev, CNPC, Hami, Peoples R China
[5] China Petr & Chem Corp, Northwest Branch Co, Urumqi, Peoples R China
[6] PetroChina Southwest Oil & Gasfield Co, Shale Gas Res Inst, Chengdu, Peoples R China
[7] Xian Shiyou Univ, Sch Earth Sci & Engn, Xian 710065, Peoples R China
[8] Northeast Petr Univ, Key Lab Continental Shale Hydrocarbon Accumulat &, Minist Educ, Daqing 163318, Peoples R China
基金
中国国家自然科学基金;
关键词
laminated shale; Malang Sag of Santanghu Basin; oil-bearing property; pore structure; shale oil; NUCLEAR-MAGNETIC-RESONANCE; RELAXOMETRY; ENRICHMENT;
D O I
10.1002/gj.4904
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Exploration and development effects of Lucaogou Formation laminated shale are not ideal in the Santanghu Basin, and the reasons are not clear. Therefore, in this study, laminated and massive shales were systematically sampled, and experiments of cryogenic adsorption of nitrogen and multi-dimensional nuclear magnetic resonance comparison were carried out. The results show that Lucaogou Formation shale is rich in volcanic ash and low content of clay, which can be divided into tuff, dolomite, tuffaceous dolomite, dolomitic tuff, and other lithologic types. The laminar structure is developed in tuffaceous dolomite and dolomitic tuff. The pores of Lucaogou Formation shale with a diameter of more than 10 nm can be used as an effective storage space for movable oil. The oil saturation and mobile oil ratio of laminated shale are lower than that of massive shale. Movable oil is controlled by carbonate content, and the higher the content, the higher the proportion of movable oil. Millimetre laminae are rich in organic matter and have poor interlaminar pore connectivity, which leads to strong adsorption capacity for oil. Therefore, the migration of oil between laminae is blocked, and oil mainly distributes or migrates in the bedding plane between laminae in laminated shale, which cannot be used as favourable reservoirs.
引用
收藏
页码:980 / 999
页数:20
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