石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (6): 1414-1422.doi: 10.11743/ogg20210615
陈维涛1(), 徐少华2,*(), 孙珍3, 何敏1, 姚佳利1, 王英民4, 卓海腾5
收稿日期:
2020-04-20
出版日期:
2021-12-28
发布日期:
2021-12-16
通讯作者:
徐少华
E-mail:chenwt2@cnooc.com.cn;xsh_xu@163.com
第一作者简介:
陈维涛(1983—), 男, 高级工程师, 石油地质勘探。E-mail: 基金项目:
Weitao Chen1(), Shaohua Xu2,*(), Zhen Sun3, Min He1, Jiali Yao1, Yingmin Wang4, Haiteng Zhuo5
Received:
2020-04-20
Online:
2021-12-28
Published:
2021-12-16
Contact:
Shaohua Xu
E-mail:chenwt2@cnooc.com.cn;xsh_xu@163.com
摘要:
层序地层学标准化理论在陆架坡折-陆坡深水区的应用尚未成熟。截至目前,基于浅层高分辨率地震和露头资料对深水层序开展的研究大多聚焦于深水水道或盆底扇内部,而忽视了与上陆坡以及陆架体系的系统对比。将层序地层学标准化理论应用于珠江口盆地中中新世(13.8 Ma前后)的陆架坡折到陆坡区,通过三维地震资料的系统解释、属性提取、可视化和钻测井信息分析,建立了从陆架到陆坡区的统一层序地层格架。在此基础上,明确了珠江口盆地陆架坡折-陆坡深水区中中新世沉积层序具有海侵体系域和高位体系域厚度薄、强制海退体系域和低位体系域前积层厚度大,以及底积层(主要为深水扇)普遍发育于低位体系域的层序地层发育特征。深水区层序地层格架的建立应从陆架坡折区到深水区整体考虑,结合“源-汇”体系演化特征进行三维空间的系统对比,才能准确划分各个体系域,从而更好地认识陆架-陆坡-深水区的沉积耦合关系。
中图分类号:
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