Prediction of exploration targets based on integrated analyses of source rock and simulated hydrocarbon migration direction: a case study from the gentle slope of Shulu Sag, Bohai Bay Basin, northern China

被引:4
作者
Ren, Changqing [1 ,2 ]
He, Fugui [1 ,2 ]
Gao, Xianzhi [1 ,2 ]
Wu, Dongsheng [3 ]
Yao, Wenli [4 ]
Tian, Jianzhang [5 ]
Guo, Huiping [5 ]
Huang, Yuanxin [5 ]
Wang, Li [5 ]
Feng, Han [6 ]
Li, Junwei [7 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Coll Geosci, 18 Fuxue Rd, Beijing 102249, Peoples R China
[3] Yangtze Univ, Coll Geosci, Wuhan 430100, Hubei, Peoples R China
[4] Yangtze Univ, Engn & Technol Coll, Jingzhou 434020, Hubei, Peoples R China
[5] PetroChina, Huabei Oilfield Branch Co, Renqiu 062550, Hebei, Peoples R China
[6] Petrochina, Nanpu Oilfield Operat Distr Jidong Oilfield Co, Tangshan 063200, Hebei, Peoples R China
[7] China Natl Offshore Oil Corp, Tianjin Branch Co, Tianjin 300452, Peoples R China
关键词
Shulu Sag; gentle slope; source rock; hydrocarbon migration; preferred hydrocarbon accumulation site; TARIM BASIN; FLUID-FLOW; OIL; ACCUMULATION; DEPRESSION; FAULT;
D O I
10.1007/s12303-018-0078-0
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Shulu Sag which is a rifted sag with NNE trend is located in the south of Jizhong Depression, Bohai Bay Basin, northern China. The gentle slope and three troughs are situated in the west and east of the sag, respectively. Both of the lower part of Shasan Member (Es3x) and the lower part of Shayi Member (Es1x) act as source rocks in this sag. Researches on the type, quantity, quality and thermal maturity of the respective organic matter have been conducted using Rock-Eval pyrolysis data. Type II is the dominant kerogen in Es1x of all troughs. However, Type II1 and III is the dominant kerogen in Es3x of Middle-Southern and Northern trough, respectively. TOC (total organic carbon) and pyrolysis S-2 (hydrocarbon) values suggest that the Es1x source rocks in Middle-Southern and Northern trough are fair to good and poor to fair generative potential of hydrocarbon, separately. The Es3x source rocks in Middle-Southern and Northern trough possess fair to excellent and poor to fair generative potential of hydrocarbon, individually. T-max (pyrolysis temperature at maximum S-2) values indicate that most of Es3x samples are thermally mature, but all Es1x samples are thermally immature. Under large scale condition, the hydrocarbon secondary migration in the upper part of Shasan Member (Es3s), Shaer Member (Es2) and the upper part of Shayi Member (Es1s) have been simulated using fluid potential model with Arcgis 9.3 software. The simulation results reveal the direction of hydrocarbon secondary migration and the distribution of hydrocarbon migration-accumulation units (HMAUS), and also suggest that the hydrocarbon migration direction is obviously controlled by nose-like structure belts where most of hydrocarbons accumulate. That shows high reliability because they are consistent with the hydrocarbon exploration result in this area. On the basis of integrated analyses of source rocks and hydrocarbon migration direction, the following five areas in the gentle slope are identified to be the preferred hydrocarbon accumulation area: Taijiazhuang area, northern and southern Xicaogu area, as well as northern and southern Leijiazhuang area. It is considerably helpful to reduce the risk in hydrocarbon exploration of Shulu Sag.
引用
收藏
页码:977 / 989
页数:13
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