Effect of Salinity on Source Rock Formation and Its Control on the Oil Content in Shales in the Hetaoyuan Formation from the Biyang Depression, Nanxiang Basin, Central China

被引:58
作者
He, Taohua [1 ,2 ]
Lu, Shuangfang [1 ]
Li, Wenhao [1 ]
Tan, Zhaozhao [1 ,2 ]
Zhang, Xinwen [3 ]
机构
[1] China Univ Petr East China, Res Inst Unconvent Oil & Gas & Renewable Energy, Qingdao 266580, Shandong, Peoples R China
[2] China Univ Petr East China, Sch Geosci, Qingdao 266580, Shandong, Peoples R China
[3] Henan Oilfield Co, SINOPEC, Res Inst Explorat & Dev, Zhengzhou 450000, Henan, Peoples R China
基金
中国国家自然科学基金;
关键词
BOHAI BAY BASIN; ORGANIC-MATTER; ARGILLACEOUS DOLOMITE; TARIM BASIN; GEOLOGICAL CHARACTERISTICS; EVALUATION CRITERIA; FORMATION MECHANISM; JIANGHAN BASIN; GEOCHEMISTRY; SAG;
D O I
10.1021/acs.energyfuels.8b01075
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
A total of 75 shale samples from the Biyang Depression were analyzed with Rock-Eval, total organic carbon (TOC), organic maceral, and gas chromatographymass spectrometry (GCMS) techniques to reveal the effect of salinity on source rock formation and its control on the oil content. On the basis of the diversities in salinity and redox conditions reflected by the gammacerane/alpha beta C-30 hopane (G/H) ratio, the pristine/phytane (Pr/Ph) ratio, and the extended tricyclic terpane ratio [ETR = (C-28 + C-29) tricyclic terpane/Ts)], three types (T1, T2, and T3) of shales were identified, which deposited in the brackish condition (G/H ratio < 0.3), the semi-saline condition (G/H ratio = 0.30.6), and the saline condition (G/H ratio > 0.6), respectively. The comparisons among T1, T2, and T3 shales revealed that the salinity had a significant effect on the paleoproductivity of the lacustrine system. Most algae thrive in semi-saline conditions (T2) but are restrained in saline conditions (T3), so that moderate salinity conditions (G/H ratio = 0.30.6) are most conducive to the accumulation of algae organic matter (AOM). Although they have similar thermal maturity (0.61.1% vitrinite reflectance) and kerogen type (type II), the T1, T2, and T3 shales were developed in different reducing environments indicated by the Pr/Ph ratio and contained variable abundance of organic matter, resulting in remarkable differences in the preservation condition of AOM and the shale oil content within the T1, T2, and T3 shales. The classification and evaluation criteria of the shale oil resource were performed according to three categories based on the oil content (S-1) and TOC values. It was revealed that the T1, T2, and T3 source rocks were mainly distributed among these areas of the potential, enriched, and ineffective shale oil resources, respectively, suggesting that shales developed in semi-saline environments deserve to be the most desirable target of shale oil exploration and development at present. Thus, this work may help related industry practitioners acquire valuable information from lacustrine shale systems.
引用
收藏
页码:6698 / 6707
页数:10
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