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柴北缘鱼卡地区大煤沟组七段页岩岩相特征及沉积演化模式

白楠, 徐尚, 王雨轩, 郭天旭, 石万忠

白楠, 徐尚, 王雨轩, 等. 柴北缘鱼卡地区大煤沟组七段页岩岩相特征及沉积演化模式[J]. 西北地质, 2021, 54(2): 74-85. DOI: 10.19751/j.cnki.61-1149/p.2021.02.006
引用本文: 白楠, 徐尚, 王雨轩, 等. 柴北缘鱼卡地区大煤沟组七段页岩岩相特征及沉积演化模式[J]. 西北地质, 2021, 54(2): 74-85. DOI: 10.19751/j.cnki.61-1149/p.2021.02.006
BAI Nan, XU Shang, WANG Yuxuan, et al. Facies Characteristics and Sedimentary Evolution Model of the 7thMember of Dameigou Formation in Yuqia Area, North Qaidam Basin[J]. Northwestern Geology, 2021, 54(2): 74-85. DOI: 10.19751/j.cnki.61-1149/p.2021.02.006
Citation: BAI Nan, XU Shang, WANG Yuxuan, et al. Facies Characteristics and Sedimentary Evolution Model of the 7thMember of Dameigou Formation in Yuqia Area, North Qaidam Basin[J]. Northwestern Geology, 2021, 54(2): 74-85. DOI: 10.19751/j.cnki.61-1149/p.2021.02.006

柴北缘鱼卡地区大煤沟组七段页岩岩相特征及沉积演化模式

基金项目: 

国家自然科学基金项目(41690134,41821002);山东省重点研发计划(2020ZLYS08);中国石油大学(华东)自主创新科研计划(21CX06001A)。

详细信息
    作者简介:

    白楠(1996-),男,在读硕士研究生,主要从事非常规油气方面研究工作。E-mail:893671588@qq.com。

    通讯作者:

    徐尚(1985-),男,副教授,主要从事油气成藏机理和非常规油气地质方面的研究工作。E-mail:xushang0222@163.com。

  • 中图分类号: P618.12

Facies Characteristics and Sedimentary Evolution Model of the 7thMember of Dameigou Formation in Yuqia Area, North Qaidam Basin

  • 摘要: 近年来,中国陆相盆地页岩油成为油气勘探开发的热点和难点。笔者以柴达木盆地北缘鱼卡地区中侏罗统大煤沟组七段为研究对象,通过岩心、普通薄片观察、有机地化、X衍射等实验,研究了大煤沟组七段的岩相特征、沉积演化模式,为优质烃源岩的发育分布提供理论依据。研究结果表明,该段共发育6种岩相,垂向上可划分为3个沉积阶段。阶段A为温湿气候下的三角洲前缘、浅湖环境,发育贫有机质块状黏土质、硅质泥岩相,强陆源输入导致水体富氧,使该阶段页岩油气潜力较差,TOC平均为0.79%;阶段B为构造沉降作用下半深湖-深湖环境,发育富有机质块状黏土质泥岩相,深湖还原环境为有机质提供了良好保存条件,使该阶段页岩油气潜力较高,TOC平均为4.16%;阶段C为干旱气候、构造沉降共同控制的半深湖-深湖环境,发育富有机质纹层状钙质、富黏土钙质、黏土质泥岩相,湖水咸化分层提供了良好的有机质保存条件,适应性藻类勃发提供了高生产力,使该阶段页岩油气潜力最高,TOC平均为5.03%。
    Abstract: In recent years, shale oil incontinental basins of China has become a hotspot in oil and gas exploration and development.This paper studied the lithofacies characteristics and sedimentary evolution model of the 7th member of Dameigou formation of Middle JurassicinYuqia area, north Qaidam Basin by means of observation of core and thin section, organic geochemistry and X-ray diffraction experiments.It provided theoretical basis for the development and distribution of high-quality source rocks.The results show that there are six types of lithofacies, which can be divided into three sedimentary stagesin the vertical direction.Stage A is the delta front and shallow lake sedimentary environment under warm and humid climate,which develops massive poor-organicclay and siliceous mudstone facies.Strong terrestrial input leads to the oxygen-rich water bodywith an average TOC of 0.79%.Therefore, shale oil and gas potential is poor at this stag.Stage B is a semi-deep to deep lake sedimentary environment under tectonic subsidence, which develops the massive rich organic clay mudstone facies.The deep-lakereducing environment provides good condition for the preservation of organic matter.A higher potential of oil and gas appears with an average TOC of 4.16%.Stage C is a semi-deep to deep lake sedimentary environment jointly controlled by arid climate and tectonic subsidence, which develops the laminar calcareous organic-rich matter,calcareous clay-rich and clayey mudstone facies.Good preservation conditions of organic matter by lake salinity stratification and high productivity of adaptive alga make stage C the highest shale oil and gas potential with an average TOC of 5.03%.
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  • 收稿日期:  2020-10-04
  • 修回日期:  2020-11-08
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