石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (4): 838-851.doi: 10.11743/ogg20200416

• 油气地质 • 上一篇    下一篇

苏北地区早寒武世黑色页岩地球化学特征与有机质富集模式

张玉玺1,2,3(), 陈建文2,3, 周江羽1   

  1. 1. 中国地质大学(武汉) 资源学院, 湖北 武汉 430074
    2. 中国地质调查局 青岛海洋地质研究所, 山东 青岛 266071
    3. 青岛海洋科学与技术试点国家实验室 海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071
  • 收稿日期:2019-11-19 出版日期:2020-08-01 发布日期:2020-08-11
  • 作者简介:张玉玺(1981-),女,博士研究生,石油地质。E-mail:zhyx0829@163.com
  • 基金资助:
    自然资源部中国地质调查局项目(DD20160152);自然资源部中国地质调查局项目(DD20190818);国家自然科学基金项目(41702162);山东省自然科学基金项目(ZR2019BD067)

Geochemical features and organic matter enrichment in the Early Cambrian black shale, northern Jiangsu area

Yuxi Zhang1,2,3(), Jianwen Chen2,3, Jiangyu Zhou1   

  1. 1. School of Earth Resources, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China
    2. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, Shandong 266071, China
    3. Pilot National Laboratory for Marine Science and Technology(Qingdao), Laboratory for Marine Mineral Resources, Qingdao, Shandong 266071, China
  • Received:2019-11-19 Online:2020-08-01 Published:2020-08-11

摘要:

早寒武世期间沉积的一套富有机质页岩,沉积厚度大,有机质含量高,是目前华南地区海相页岩气勘探重要目标层系之一。以苏北地区XYZ-1为例,利用钻井岩心资料和地球化学测试分析数据,探讨早寒武世幕府山组黑色页岩的沉积环境及有机质富集模式研究。结果表明,XYZ-1井幕府山组为一套黑色、深灰色炭质页岩夹薄层状碳酸盐岩的沉积层序,顶部和底部发育有石煤层。幕府山组V/(Ni+V)平均值为0.74,Ni/Co的平均值为6.78,U/Th的平均值为1.46,V/Sc的平均值为65.43,氧化还原指标表明幕府山组整体为缺氧的沉积环境,在底部和顶部存在两次较为强烈的硫化事件。幕府山组炭质页岩的TOC平均值为5.62%,其中72.2%的样品大于2%,TOCTS相关系数高达0.89。因此,缺氧的沉积条件为有机质的富集和保存提供了保障,硫化的沉积环境是有机质富集的关键因素,苏北地区幕府山组具备了发育良好烃源岩和储层的条件。

关键词: 有机质富集, 黑色页岩, 幕府山组, 早寒武世, 苏北地区

Abstract:

A set of black shale deposited in the Early Cambrian and characterized by a large thickness and high organic matter content is one of the important exploration target strata for marine shale gas in South China.The sedimentary environment and enrichment mechanism of organic matters in the black shale are discussed based on the core and geochemical data from Well XYZ-1 drilled through the Early Cambrian Mufushan Formation in northern Jiansu area.The Mufushan Formation in Well XYZ-1 is a set of depositional sequence of black and dark gray carbonaceous shale with stone coal layers on top and at bottom and interbeds of thin-layered carbonate rocks.The average values of V/(Ni+V), Ni/Co, U/Th, and V/Sc are 0.74, 6.78, 1.46, and 65.43, respectively.These ratios as indicators of redox environment suggest that the sediments were under anoxic conditions and two strong sulfidation events once occurred at the bottom and top.The average total organic carbon (TOC) content of the Mufushan carbonaceous shale is 5.62%, with the TOC value of 72.2% of the samples collected greater than 2%.The TOC-TS correlation coefficient is as high as 0.89.The hypoxic environment with sulfidation events provided favorable conditions for the enrichment and preservation of organic matters, thus laid down foundation for the development of high-quality source rocks and reservoirs in the Mufushan Formation of northern Jiansu.

Key words: enrichment of organic matter, black shale, Mufushan Formation, Early Cambrian, northern Jiangsu area

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