A new method for continental shale oil enrichment evaluation

2017 ◽  
Vol 5 (2) ◽  
pp. T209-T217 ◽  
Author(s):  
Siyuan Su ◽  
Zhenxue Jiang ◽  
Zhiye Gao ◽  
Chuanxiang Ning ◽  
Zhi Wang ◽  
...  

We have evaluated continental shale oil enrichment via experiments. Rock pyrolysis, nuclear magnetic resonance, and pulse permeability tests were conducted to establish the pore saturation index (PSI), which comprehensively evaluates the enrichment of shale oil features using the characteristics of self-generation and self-preservation, the parameters of which include the pyrolysis-free hydrocarbon ([Formula: see text]) and total organic carbon of source rocks as well as the porosity and permeability of reservoir rocks. The correlation of the oil content ([Formula: see text]) and PSI values indicated that PSI values greater than 50 generally indicate good oil enrichment plays, whereas those smaller than 50 imply poor conditions for oil enrichment. This conclusion was successfully applied to the Zhanhua Sag with shale oil plays in the Jiyang Depression, Bohai Bay Basin, China. In addition, the shale oil plays of the Dongying Sag in the Jiyang Depression were investigated to verify the effectiveness and reliability of the new method.

2014 ◽  
Vol 41 (6) ◽  
pp. 703-711 ◽  
Author(s):  
Linye ZHANG ◽  
Youshu BAO ◽  
Juyuan LI ◽  
Zheng LI ◽  
Rifang ZHU ◽  
...  

2018 ◽  
Vol 6 (4) ◽  
pp. SN11-SN21
Author(s):  
Zhenkai Huang ◽  
Maowen Li ◽  
Quanyou Liu ◽  
Xiaomin Xie ◽  
Peng Liu ◽  
...  

Systematic organic petrology and geochemistry analyses have been conducted in the source rocks of the lower Es3 and upper Es4 members of the Shahejie Formation in the Niuzhuang Sub-sag, Jiyang Depression, Bohai Bay Basin, eastern China. The results indicate that the main organic types of shale and nongypsum mudstone in the lower Es3 and upper Es4 member are I-II1 kerogen, and the predominant ([Formula: see text]) activation energy frequencies range from 57 to [Formula: see text]. The similar distribution characteristics in the two source rocks indicate that they have a similar hydrocarbon maturation process. An extensive pyrolysis analysis indicates that the source rocks of the upper Es4 member do not have an obvious double peak hydrocarbon generation model. Previous studies indicate that the hydrocarbon index peak at a depth of 2500–2700 m is affected by migrating hydrocarbon. Major differences are not observed in the hydrocarbon generation and evolution process of the shale and nongypsum mudstone. The primary oil generation threshold of the lower Es3 and upper Es4 members is approximately 3200 m, and the oil generation peak is approximately 3500 m. The activation energy distribution of the gypsum mudstone of the upper Es4 member is wider than that of the shale and nongypsum mudstone, and lower activation energies account for a larger proportion of the activation energies. The above factors may lead to a shallower oil generation threshold for gypsum mudstone compared with that for shale and nongypsum mudstone.


2016 ◽  
Vol 43 (5) ◽  
pp. 759-768 ◽  
Author(s):  
Yong WANG ◽  
Xuejun WANG ◽  
Guoqi SONG ◽  
Huimin LIU ◽  
Deshun ZHU ◽  
...  

2016 ◽  
Vol 1 (1) ◽  
pp. 70-80 ◽  
Author(s):  
Yongshi Wang ◽  
Zheng Li ◽  
Jianqiang Gong ◽  
Jiajun Zhu ◽  
Yunqing Hao ◽  
...  

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