天然气勘探

地震属性在马仙地区下干柴沟组下段沉积环境分析中的应用

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  • 1.中国科学院油气资源研究重点实验室,甘肃 兰州 730000;
    2.中国石油青海油田公司勘探开发研究院,甘肃 敦煌 736202;
    3.中国石油青海油田天然气开发公司,青海 格尔木 816000
孙国强(1977-),男,河南洛阳人,副研究员,博士,主要从事含油气盆地石油地质学及沉积构造研究. E-mail:sguoqiang@lzb.ac.cn.

收稿日期: 2013-05-29

  修回日期: 2013-07-06

  网络出版日期: 2013-12-10

基金资助

中国科学院2012年度“西部之光”人才计划支持项目;中国科学院油气资源研究重点实验室开放基金项目(编号:KFJJ2012-05)联合资助.

Application of Seismic Attributes to Analysis of Depositional Environment:Taking Lower Member of Xiaganchaigou Formation of the Paleogene System of Maxian Region as an Example

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  • 1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000,China;2.Exploratory Development Institute of Qinghai Petroleum Administration,Dunhuang 736202,China;3.The Second Oil Production Factory in Qinghai Oilfield,Germu 816000,China

Received date: 2013-05-29

  Revised date: 2013-07-06

  Online published: 2013-12-10

摘要

在对20多口钻井的录井资料、岩心特征、粒度特征、测井资料及沉积层序分析的基础上,研究了柴达木盆地北缘西段马仙地区古近系下干柴沟组下段的沉积特征及演化规律。结果表明:研究区古近系下干柴沟组下段的沉积环境主要是以辫状河河流相的心滩、河漫滩、泛滥平原为主,在下干柴沟组下段沉积时期为一明显的水进过程。三维地震数据精细构造解释基础上的地震属性研究也很好地反映了研究区下干柴沟组下段沉积时期沉积环境的变化规律:早期以东北部的物源为主,正北方只有少量物源供给,砂体主要受东北部物源控制;之后东北部物源向西迁移,供给量逐渐减小,北部物源供给量逐渐增大;晚期2个物源逐渐靠近,河流相砂体呈连片分布。结合区域地质分析初步弄清了下干柴沟组下段沉积环境的演化过程,明确了3套砂体的分布规律,为柴北缘马仙地区下一步的油气勘探工作提供了可靠的地质依据。

本文引用格式

孙国强,马进业,司丹,王海峰,王珑,史基安 . 地震属性在马仙地区下干柴沟组下段沉积环境分析中的应用[J]. 天然气地球科学, 2013 , 24(6) : 1246 -1252 . DOI: 10.11764/j.issn.1672-1926.2013.06.1246

Abstract

Based on the analyses of sedimentary sequence,lithology,particle size,and logging data from more than 20 drilling wells in Maxian region on the northern margin of the Qaidam Basin,the sedimentary characteristics and its evolution of Paleogene Lower Xiaganchaigou Formation were studied.The results showed that braided fluvial facies were the main sediment types of this formation,including channel bar,point bar,and flood plain,and the environment with water withdrawal was the main depositional environment in this period.According to the fine structural interpretation of 3D seismic data,seismic attributes can also well illustrate the changes of depositional environment of the Lower Xiaganchaigou Formation:In the early period,the sediments were mainly from northeast of the Maxian region,and a little from the north,and sandbodies were mainly dominated by the northeastern provenance;Along with the basin development,the northeastern provenance gradually migrated westward,and its supplies also decreased,in contrast,the supplies from the northern provenance increased;In the later period,the above two provenances got closed,and then developed large and contiguous sandbodies.Preliminary conclusions about the environmental evolution of Lower Xiaganchaigou Formation in Maxian region and three sandbodies distribution can provide reliable geological data for the next oil and gas exploration.

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