西湖凹陷花港组浅水三角洲平原分流河道沉积构型  

Architecture characteristics of distributary channels in shallow water delta plain of the Huagang Formation in Xihu sag,East China Sea

作　　者：杨征 吴胜和[1,2] 段冬平 徐振华[1,2] 熊绮聪 张玉飞 YANG Zheng;WU Shenghe;DUAN Dongping;XU Zhenhua;XIONG Qicong;ZHANG Yufei(College of Geosciences,China University of Petroleum(Beijing),Beijing 102249,China;National Key Laboratory of Petroleum Resources and Engineering,China University of Petroleum(Beijing),Beijing 102249,China;Shanghai Branch,CNOOC(China)Co.,Ltd.,Shanghai 200335,China)

机构地区：[1]中国石油大学(北京)地球科学学院,北京102249 [2]油气资源与工程全国重点实验室,中国石油大学(北京),北京102249 [3]中海石油(中国)有限公司上海分公司,上海200335

出　　处：《古地理学报》2024年第3期525-544,共20页Journal of Palaeogeography：Chinese Edition

基　　金：国家自然科学基金项目(编号:42272110)资助。

摘　　要：渐新统花港组上段是东海陆架盆地西湖凹陷中南部地区的主要产油气层位,但对其沉积体系的认识一直存在争议,砂体构型特征及控制因素的研究也相对匮乏。综合运用岩心、测井及地震等资料,研究渐新统花港组上段沉积环境、沉积微相类型、砂体沉积构型特征及其控制因素。结果表明:西湖凹陷中南部花港组上段以浅水三角洲平原沉积为主,分流河道是最主要的砂体类型。根据弯曲度差异,可将分流河道划分为辫流型(弯曲度1~1.05)、曲流型(弯曲度大于1.15)和辫-曲转换型(弯曲度1.05~1.15)3种类型,其中辫流型分流河道砂体“宽而厚”,平面组合呈交织宽条带状,心滩呈斑点状排列,砂体垂向叠置样式以切叠型为主;曲流型分流河道砂体“窄而薄”,平面样式为单一条带型或分叉-合并型,厚砂以点坝的形式分布在河道边缘,砂体垂向叠置样式以“孤立型”为主;辫-曲转换型分流河道是辫流型和曲流型的过渡类型,河道砂体规模中等,河道内心滩和点坝同时发育。3类分流河道的厚度与宽度呈对数正相关,宽厚比具有辫流型>辫-曲转换型>曲流型的特征。推测古地貌和基准面变化是影响浅水三角洲分流河道构型特征的主要因素,其中古地貌控制了分流河道的河型变化,较陡的地形有利于低弯度辫流型分流河道的形成,而长期基准面上升造成了分流河道规模逐渐下降,中期基准面的上升造成了分流河道砂体叠置样式发生切叠型→叠加型→孤立型的演变。研究成果完善了浅水三角洲的沉积构型知识库,对地下浅水三角洲分流河道储集层的预测及开发具有重要的指导意义。The upper Oligocene Huagang Formation is crucial for oil and gas exploration in the central and southern Xihu sag of the East China Sea Shelf Basin.However,there has been ongoing debate on the sedimentary system,and limited research has been conducted on the characteristics of sand body architecture and the controlling factors.This paper studied the sedimentary environment,microfacies types,sand body architecture,and controlling factors of the upper Oligocene Huagang Formation through a comprehensive analysis of core,logging,and seismic data.The upper Huagang Formation in the central-south part of Xihu sag shows shallow-water delta plain sedimentation,with distributary channels being the predominant type of sand body.These distributary channels are categorized into three types based on their curvature:braided(curvature=1~1.05),meandering(curvature>1.15),and braided-meander transition(curvature=1.05~1.15).The sand bodies found in braided distributary channels are wide and thick,with intertwined wide bands.Channel bars in these channels are arranged in a speckled pattern.The sand body’s vertical stacking style is mainly characterized as incised stacking.In contrast,the sand bodies in meandering channels are narrow and thin,appearing as either single strip type or bifurcation-merging type in the planar direction.Thick sand layers are distributed as point bars in the channel margin,and the vertical stacking style is mostly isolated.The braided-meandering type of diversion channel is a transitional type between braided and meandering channels.It is characterized by moderate-sized channel sand bodies containing inner channel bars and point bars.The thickness and width of these distributary channels are positively correlated in a logarithmic manner.The ratio of width to thickness follows the pattern of braided type>transitional type>meandering type.The architecture characteristics of distributary channels are primarily influenced by paleogeomorphology and changes in base levels.Paleogeomorphology controls changes in c

关 键 词：东海陆架盆地 西湖凹陷 渐新统 花港组 浅水三角洲 分流河道 沉积构型 

分 类 号：P512.2[天文地球—地质学]