地质科技通报2024,Vol.43Issue(3) :81-93.DOI:10.19509/j.cnki.dzkq.tb20220705

塔里木盆地富满地区吐木休克组烃源岩有机地球化学特征及其油气勘探意义

Organic geochemical characters of source rock and significance for explo-ration of the Tumuxiuke Formation in Fuman area,Tarim Basin

杨海军 蔡振忠 李勇 杨宪彰 张银涛 张艳秋 孙冲 康鹏飞 张海祖 赵星星
地质科技通报2024,Vol.43Issue(3) :81-93.DOI:10.19509/j.cnki.dzkq.tb20220705

塔里木盆地富满地区吐木休克组烃源岩有机地球化学特征及其油气勘探意义

Organic geochemical characters of source rock and significance for explo-ration of the Tumuxiuke Formation in Fuman area,Tarim Basin

杨海军 1蔡振忠 1李勇 1杨宪彰 1张银涛 1张艳秋 1孙冲 1康鹏飞 2张海祖 1赵星星2
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作者信息

  • 1. 塔里木油田公司研发中心,新疆库尔勒 841000;中国石油天然气集团有限公司超深层复杂油气藏勘探开发技术研发中心,新疆库尔勒 841000;新疆超深油气重点实验室,新疆库尔勒 841000
  • 2. 塔里木油田公司研发中心,新疆库尔勒 841000
  • 折叠

摘要

塔里木盆地富满地区吐木休克组烃源岩作为近期勘探新发现的烃源岩层,具有良好的油气勘探前景,因此亟需对其进一步开展烃源岩地球化学评价,以便更好地指导勘探.通过总有机碳含量、岩石热解测定以及饱和烃、芳烃色谱-质谱(GC-MS)等分析方法对富满地区吐木休克组黑色泥岩及灰色泥岩岩屑样品进行了定性和定量表征.研究结果表明,吐木休克组烃源岩有机质丰度高,均值为3.4%,氢指数(HI)最高可达到590 mg/g,干酪根类型以Ⅱ型干酪根为主,为一套好-极好的优质烃源岩.从分子地球化学特征来看,烃源岩形成于弱还原偏咸水的海相沉积环境中,以低等水生藻类作为主要成烃生物.基于热解峰温Tmax及饱和烃生物标志化合物和芳香烃热成熟度参数,吐木休克组烃源岩总体处于低成熟-中等成熟阶段,具有良好的生烃潜力.富满地区东南部区域作为环满坳陷西部斜坡区,可能分布有更厚、更优的吐木休克组烃源岩,且烃源岩可能已达到更高的热演化程度,其对奥陶系油气资源的贡献不可忽视.

Abstract

[Objective]As a newly discovered source rock in the Fuman area of the Tarim Basin,the source rock of the Tumuxiuke Formation has good petroleum exploration prospects,and the geochemical evaluation of the source rock is conducive to guiding exploration.[Methods]The qualitative and quantitative characterization of drill cut-tings from the Tumuxiuke Formation in the Fuman area was carried out by means of total organic carbon(TOC)content,Rock-Eval pyrolysis,and GC-MS analysis of saturated and aromatic hydrocarbons.[Results]The results show that the source rock of the Tumuxiuke Formation is a good to excellentsource rock,with an average TOC con-tent of 3.4%.The highest hydrogen index(HI)is 590 mg/g,and the kerogen type is mainly type Ⅱ.According to the molecular geochemical characteristics,the source rock was formed in a marine sedimentary environment with weakly reducing brackish water,with aquatic algae as the primary hydrocarbon-generating organisms.Based on the peak temperature(Tmax)of Rock-Eval,saturated hydrocarbon biomarker compounds,and aromatic hydrocarbon thermal maturity parameters,the source rock of the Tumuxiuke Formation is generally in the mature-medium mature evolution stage and has good hydrocarbon generation potential.[Conclusion]As the sedimentary center of the Huanman Depression,the southern Fuman area may have thicker and higher-quality Tumuxiuke source rock with a greater degree of thermal evolution,whose contribution to the oil and gas resources in the Ordovician cannot be ig-nored.

关键词

塔里木盆地/富满地区/吐木休克组/烃源岩/有机地球化学

Key words

Tarim Basin/Fuman area/Tumuxiuke Formation/source rock/organic geochemistry

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基金项目

中国石油科学研究与技术开发项目(2021DJ1501)

出版年

2024
地质科技通报
中国地质大学(武汉)

地质科技通报

CSTPCDCSCD北大核心
影响因子:1.018
ISSN:2096-8523
被引量1
参考文献量13
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