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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

机译:盐度对华中地区南阳盆地碧阳pression陷河套源组页岩含油量的影响及其对页岩含油量的控制

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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.
机译:利用岩石评估,总有机碳(TOC),有机显微法和气相色谱质谱(GCMS)技术对the阳yang陷的75个页岩样品进行了分析,以揭示盐度对烃源岩形成的影响及其对成岩作用的控制。含油量。根据盐度和氧化还原条件的多样性,由γ-角cer烷/αβC-30 hop烷(G / H)比,原始/植烷(Pr / Ph)比和扩展的三环萜烯比[ETR =( (C-28 + C-29)三环萜烯/ Ts)],确定了三种类型的页岩(T1,T2和T3),这些页岩沉积在半咸水条件(G / H比<0.3),半盐条件下(G / H比= 0.30.6)和盐水条件(G / H比> 0.6)。 T1,T2和T3页岩的比较表明,盐度对湖相系统的古生产力具有显着影响。大多数藻类在半盐条件下(T2)繁盛,但在盐水条件下(T3)受抑制,因此中等盐度条件(G / H比= 0.30.6)最有利于藻类有机质(AOM)的积累。尽管它们具有相似的热成熟度(0.61.1%镜质体反射率)和干酪根类型(II型),但T1,T2和T3页岩在Pr / Ph比所指示的不同还原环境中发育,并且含有丰富的有机质,导致T1,T2和T3页岩的AOM保存条件和页岩含油量存在显着差异。根据含油量(S-1)和总有机碳(TOC)值,根据三类页岩油资源的分类和评价标准。结果表明,T1,T2和T3烃源岩分别主要分布在潜在,富集和无效页岩油资源的这些区域中,这表明在半盐环境中开发的页岩应成为最理想的目标。目前页岩油的勘探开发。因此,这项工作可以帮助相关行业从业者从湖相页岩系统中获取有价值的信息。

著录项

  • 来源
    《Energy & fuels》 |2018年第6期|6698-6707|共10页
  • 作者单位

    China Univ Petr East China, Res Inst Unconvent Oil & Gas & Renewable Energy, Qingdao 266580, Shandong, Peoples R China;

    China Univ Petr East China, Res Inst Unconvent Oil & Gas & Renewable Energy, Qingdao 266580, Shandong, Peoples R China;

    China Univ Petr East China, Res Inst Unconvent Oil & Gas & Renewable Energy, Qingdao 266580, Shandong, Peoples R China;

    China Univ Petr East China, Res Inst Unconvent Oil & Gas & Renewable Energy, Qingdao 266580, Shandong, Peoples R China;

    Henan Oilfield Co, SINOPEC, Res Inst Explorat & Dev, Zhengzhou 450000, Henan, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-18 00:39:09

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