地学前缘 ›› 2018, Vol. 25 ›› Issue (4): 210-225.DOI: 10.13745/j.esf.sf.2018.6.26

• 盆地与资源 • 上一篇    下一篇

广域电磁法在洞庭盆地北部生物气勘探中应用及远景靶区预测

孙春岩,唐侥,赵浩,张仕强,王栋琳,贺会策,凌帆,李建华,贺岩   

  1. 1. 中国地质大学(北京) 工程技术学院, 北京 100083
    2. 中南大学 地球科学与信息物理学院, 湖南 长沙 410083
  • 收稿日期:2017-10-14 修回日期:2018-03-07 出版日期:2018-07-15 发布日期:2018-07-15
  • 作者简介:孙春岩(1952—),女,教授,博士生导师,长期从事石油天然气及海洋天然气水合物地球化学勘查技术方法的理论与应用的教学和科研工作。E-mail:suncy@cugb.edu.cn
  • 基金资助:
    国家自然科学基金项目(41276056);国家高技术研究发展计划“863”项目(2013AA09A411)

Application of widefield electromagnetic method to biogas exploration and prediction of prospective target area in the northern Dongting Basin.

SUN Chunyan,TANG Yao,ZHAO Hao,ZHANG Shiqiang,WANG Donglin,HE Huice,LING Fan,LI Jianhua,HE Yan   

  1. 1. School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China
    2. School of Geosciences and InfoPhysics, Central South University, Changsha 410083, China
    3. ENN Coal Gasification Mining Co., Ltd, Langfang 065001, China
    4. No.11 Gold Geological Party of PAP, Lhasa 850000, China
    5. Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 510075, China
  • Received:2017-10-14 Revised:2018-03-07 Online:2018-07-15 Published:2018-07-15

摘要: 洞庭盆地地处湘西古生界边缘,经历了中生代晚白垩世盆地基本成型和新生代断块运动为主的两期构造旋回,为终成于燕山(中生代)延续于喜马拉雅(新生代)的断陷盆地。盆内局部凹陷白垩系之上存在着持续砂泥岩沉积及第四纪河流湖泊相现代沉积,具备了形成一定规模生物气藏的地质条件。2013—2015年笔者通过洞庭盆地浅层沉积物系统地球化学勘探,基本搞清了盆地内渗漏甲烷气体异常的分布状况。根据各指标地球化学异常特征,发现洞庭盆地北部沅江凹陷北部斜坡、青树嘴—河坝镇一带是洞庭盆地内生物气资源最有可能突破的远景区。为了追索渗漏甲烷气体来源,深化地球化学异常解释评价以及浅层生物气系统研究,2015—2016年在发现的生物气远景区,部署完成5条广域电磁测深和两条汞气测量剖面。本研究旨在通过实测地球物理和地球化学综合剖面的对比研究,揭示本区第四系构造分布和地球化学异常机制,为洞庭盆地生物气资源远景和气藏靶区的预测划分提供科学依据,也为勘探第四系生物气资源方法技术的选择提供了建议。勘探成果表明:(1)本区第四系能够满足生物气系统“生储盖”条件,具有生物气资源潜力;(2)沉积物游离烃甲烷地球化学异常是下伏第四系内气体聚集沿断裂带或沉积层向表层渗漏运移所致。酸解烃指标是识别有利于生物气体生储环境的敏感因子之一;(3)洞庭盆地工区西北部,P2剖面南段和P2线北部与P3、P4剖面交汇区域,具有良好的“自生自储”型生物气藏资源远景,是本区勘探生物资源天然气最有希望的靶区;(4)洞庭湖北部工区东部,P6测线南部接近沅江凹陷中心的四季红一带,是本区寻找 “自生自储”和“下生上储”型气藏的有利地带和资源远景区;(5)浅层沉积物地球化学勘探,有利于发现与生物气有关的气体渗漏、评价下伏沉积体系特性、缩小地球物理勘探靶区。地球化学与广域电磁剖面测量的结合是勘探生物成因天然气经济快速的方法技术。

关键词: 洞庭盆地, 生物气, 广域电磁法, 汞气测量, 地球化学异常, 第四系, 游离烃, 酸解烃

Abstract: The Dongting Basin, located at the edge of the Paleozoic in Xiangxi, experienced two stages of tectonic cycles involving mainly the Mesozoic Late Cretaceous basin and the Cenozoic fault block. This rift basin is a result of the Yanshan (Mesozoic) and Himalayan (Cenozoic) movements. There are persistent sand and shale deposits on the Cretaceous in the basin, making the sedimentary facies of the Quaternary rivers and lakes geologically favorable for biogas generation. Based on the 20132015 geochemical exploration of the shallow sediments in the Dongting Basin, we have a clear understanding of the distribution of methane gas anomalies in the basin. The geochemical anomalies indicated that the Dongting Basin biogas resources, on the northern slopes of the Yuanjiang depression in the northern Dongting Basin, QingshuzuiHebazhen area, present the most likely prospective breakthroughs. In order to trace the source of methane gas leakage, and advance our understanding of geochemical anomaly and shallow biogas system research, we completed five widearea electromagnetic sounding and two mercury gas measurement profiles in the biogas prospective area discovered in 20152016. This accomplishment was aimed to reveal the Quaternary tectonic distribution and geochemical anomaly mechanism through the comparative study of integrated geophysical and geochemical profiles. It provided a scientific basis for the Dongting Basin biogas resource prospecting and target prediction as well as guidance for the selection of Quaternary gas prospecting methodology. The results showed: (1) The Quaternary system in Dongting area can satisfy the “sourcereservoircap” condition of biogas system and has biogas resource potential; (2) The sediment free methane anomaly is caused by the Quaternary gas accumulation along the fault zone or by leakage due to the sediment layer movement towards earth surface; (3) The area encompassing the northwestern Dongting Basin, southern P2 section, and the intersection of northern P2 line and P3/P4 sections, have good “selfgeneration and selfstorage” capability, and are the most promising targets in the prospective area; (4) The Sijihong area, located in the eastern prospective area of northern Dongting Lake, along the southern P6 line and near the Yuanjiang depression center, possesses favorable conditions to form the socalled “selfgeneration and selfstorage” and “lowergeneration and upperstorage” biogas deposits; (5) Shallow sedimentary geochemical exploration is conducive to the discovery of gas leakage associated with biogas, and it is also useful in evaluating underlying depositional system, reservoir development and characterization, and targeting geophysical exploration areas. The combination of geochemistry and widearea electromagnetic profile measurements provides a fast and economical means of biogas prospecting.

Key words: Dongting Basin, biogas, wide-field electromagnetic method, mercury gas measurement, geochemical anomaly, Quaternary, free hydrocarbon, acid hydrolysis

中图分类号: