岩性油气藏 ›› 2020, Vol. 32 ›› Issue (6): 109–119.doi: 10.12108/yxyqc.20200610

• 油气地质 • 上一篇    下一篇

吉木萨尔凹陷二叠系芦草沟组烃源岩沉积古环境

蒋中发1, 丁修建2, 王忠泉1, 赵辛楣1   

  1. 1. 中国石油新疆油田分公司 勘探开发研究院, 新疆 克拉玛依 834000;
    2. 中国石油大学 (华东)地球科学与技术学院, 山东 青岛 266580
  • 收稿日期:2020-01-14 修回日期:2020-04-03 出版日期:2020-12-01 发布日期:2020-10-30
  • 通讯作者: 丁修建(1986-),男,博士,副教授,主要从事石油地质学方面的教学与科研工作。Email:dingxj@upc.edu.cn。 E-mail:dingxj@upc.edu.cn
  • 作者简介:蒋中发(1994-),男,硕士,主要从事油气地质勘探方面的研究工作。地址:(834000)新疆克拉玛依市克拉玛依区准噶尔路29号新疆油田公司勘探开发研究院。Email:jzfkts@petrochina.com.cn
  • 基金资助:
    中国石油天然气集团公司新疆重大科技专项“准噶尔盆地油藏富集规律及勘探技术与应用”(编号:2017E-0401)资助

Sedimentary paleoenvironment of source rocks of Permian Lucaogou Formation in Jimsar Sag

JIANG Zhongfa1, DING Xiujian2, WANG Zhongquan1, ZHAO Xinmei1   

  1. 1. Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    2. School of Geosciences, China University of Petroleum(East China), Qingdao 266580, Shandong, China
  • Received:2020-01-14 Revised:2020-04-03 Online:2020-12-01 Published:2020-10-30

摘要: 为查明准噶尔盆地吉木萨尔凹陷中二叠统芦草沟组烃源岩古沉积环境演化过程,对27块烃源岩样品进行主量元素、微量元素测试,并结合生物标志物、碳酸盐岩δ18O数据,对芦一段、芦二段沉积期的古氧相、古盐度、古气候以及古水深演化进行了研究。结果表明:吉木萨尔凹陷芦草沟组一段正构烷烃主峰碳以nC17为主,相对富集伽马蜡烷,Ph,β胡萝卜烷,V,U,FeO,Sr,Mg和Ca等,碳酸盐岩δ18O偏正,为干旱气候咸化贫氧—厌氧沉积,部分层段为半咸水沉积,MnO/TiO2指示其古水深较深;芦二段正构烷烃主峰碳以nC21和nC23为主,相对富集Pr,Fe2O3,Al,Ti和C24四环萜烷等,总体为湿润气候半咸水贫氧沉积,偶尔处于干旱咸化沉积,古水深相对较浅。该研究成果表明芦一段可作为研究区下一步勘探的重点层系。

关键词: 烃源岩, 地球化学, 古环境, 中二叠统, 芦草沟组, 吉木萨尔凹陷

Abstract: In order to find out the sedimentary paleoenvironment evolution process of the source rocks of Middle Permian Lucaogou Formation in Jimsar Sag,Junggar Basin,the major element and trace element tests were carried out on 27 hydrocarbon source rock samples,and combined with biomarkers and δ18O data of carbonate rocks, the paleo-oxygen facies,paleo-salinity,paleo-climate and paleo-water depth evolution of the first and second members of Lucaogou Formation were studied. The results show that nC17 is the main peak carbon of n-alkanes in the first member of Lucaogou Formation in Jimsar Sag,and gammacerane,phytane,β-carotene,vanadium, uranium,ferrous oxide,strontian,magnesium and calcium are enriched,the δ18O of autogenic carbonate in it is higher,and the paleoenvironment is saline and anaerobic-anoxic environment under arid climate,with some strata brackish,and w(MnO)/w(TiO2)indicates that its paleo-water depth is deeper. nC21 and nC23 are the main peak carbon of n-alkanes in the second member of Lucaogou Formation in Jimsar Sag,and pristine,ferric oxide,aluminum,titanium and C24 tetracyclic terpene are enriched in it,and the paleoenvironment is generally brackish-saline and anoxic environment under humid climate,occasionally saline environment under arid climate,and its paleowater depth is shallower. The research results show that the first member of Lucaogou Formation can be regarded as the next exploration focus in the study area.

Key words: source rock, geochemistry, paleoenvironment, Middle Permain, Lucaogou Formation, Jimsar Sag

中图分类号: 

  • TE121.3
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