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基于地震相研究的三水盆地布心组沉积相再解释
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  • 英文篇名:Reinterpretation of sedimentary facies based on seismic facies of the Buxin Formation in Sanshui Basin, China
  • 作者:祝圣贤 ; 侯明才 ; 黄志发
  • 英文作者:ZHU Shengxian;HOU Mingcai;HUANG Zhifa;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology;
  • 关键词:三水盆地 ; 布心组 ; 地震相 ; 沉积相
  • 英文关键词:Sanshui Basin;;Buxin Formation;;seismic facies;;sedimentary facies
  • 中文刊名:成都理工大学学报(自然科学版)
  • 英文刊名:Journal of Chengdu University of Technology(Science & Technology Edition)
  • 机构:油气藏地质及开发工程国家重点实验室(成都理工大学);
  • 出版日期:2019-04-04 16:15
  • 出版单位:成都理工大学学报(自然科学版)
  • 年:2019
  • 期:02
  • 基金:国家科技重大专项(2017ZX05008-005-009)
  • 语种:中文;
  • 页:114-122
  • 页数:9
  • CN:51-1634/N
  • ISSN:1671-9727
  • 分类号:P618.13
摘要
通过对广东三水盆地中北部始新统布心组地震剖面反射特征分析,确定其地震相类型及平面展布特征,结合钻井资料及前人研究成果对布心组进行沉积相再解释。研究表明:布心组沉积期由盆地周缘的高能地震相向盆地逐渐转变为较稳定的低能相,但盆地中部存在指示沉积环境水动力较强的地震相,说明其沉积相展布与前人以布心组为一个Ⅲ级层序划分出的滨湖-浅湖-半深湖-深湖相带分布不甚相同。三水盆地布心组沉积期滨-浅湖相发育于盆地大部,中部发育湖底扇,周缘多发育湖泊三角洲相,随时间的推移湖盆存在扩张后又收缩变浅的过程。
        Based on the analysis of seismic profile reflection characteristics, combined with the logging data and previous research results, the type of seismic facies and distribution characteristics of the Buxin Formation in the middle-northern Sanshui Basin of Guangdong Province are determined and its sedimentary facies are reinterpretated. It shows that the high-energy seismic facies in the basin periphery change into stable low-energy facies toward the center of basin. The seismic facies in the middle basin display strong hydrodynamic environments character, different from previous views which considered it as a classic third-order sequence with sedimentary facies distribution of lakeside-shallow lake-semi deep lake-deep lake. It reveals that lakeside-shallow lake deposition developed in most of the basin, sublacustrine fan occurred in the middle part of the basin, while lacustrine delta facies mainly developed in the periphery of the basin during the deposition of Buxin Formation. With the passage of time, the basin experienced expansion followed by shrinking and shallowing.
引文
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