珠江口盆地荔湾3-1气田珠江组深水扇沉积相分析  

Facies and Depositional Model of A Deepwater Fan in the Zhujiang Formation,Liwan 3-1 Gasfield,Baiyun Sag,Pearl River Mouth Basin

作　　者：李云[1] 郑荣才[1] 朱国金 高博禹 胡晓庆 

机构地区：[1]成都理工大学"油气藏地质及开发工程"国家重点实验室,成都610059 [2]中国海洋石油研究中心,北京100027

出　　处：《沉积学报》2011年第4期665-676,共12页Acta Sedimentologica Sinica

基　　金：国家重大专项"南海深水油气勘探开发示范工程-荔湾3-1气田总体开发方案及基本设计技术"子项目"深水扇储层层序地层和沉积模式研究"(编号2008ZX05056-02-02)部分研究成果

摘　　要：根据已钻井取芯段岩相分析,从荔湾3-1气田珠江组深水扇沉积体系中划分出巨厚层和厚层块状砂岩相、厚层正粒序砂岩相、厚层逆粒序砂岩相、平行—板状斜层理砂岩相、滑塌变形砂岩相、薄层砂岩夹层相、薄层(粉)砂岩与泥岩互层相、厚层粉砂岩相、厚层泥岩相和层状深水灰岩相等10种岩相类型和识别出砂岩相组合、泥岩相组合、(粉)砂岩与泥岩互层相组合、粉砂岩相组合和深水灰岩相组合等5种岩相组合类型,在此基础上,从珠江组深水扇沉积体系中进一步识别出内扇主水道、中扇分支水道、水道间、天然堤—溢岸、外扇和盆地等微相类型,将珠江组下部确定为以砂岩相组合为主的盆底扇内扇和斜坡扇内-中扇沉积组合,其中内扇主水道和中扇分支水道是最有利储层发育的沉积微相。中、上部确定为以泥岩相组合为主的外扇和盆地沉积组合,具有随海侵扩大,深水扇最终被远洋所取代的沉积演化特征。Based on detailed analysis of cores,logs,and seismic data,ten lithofacies were indentified,including mega-thick and thick massive sandstones,thick normal-graded sandstones,thick inverse-graded sandstones,parallel and tabular cross-stratified sandstones,slumped and deformed sandstones,thin sandstone interlayers,thin mudstone-sandstone interbeds,thick siltstones,thick mudstones,and deep-water limestones.They can be organized into five lithofacies associations.These are sandstone-dominated,mudstone-dominated,mudstone-sandstone interbed,siltstone and deep-water limestone associations.Based on the analyses of lithofacies and their associations,the depositional system of the reservoir in the Zhujiang Formation,Liwan 3-1 field is identified as submarine fan.Four microfacies are further recognized within the fan based on detailed analysis,including channels（including main channels in the inner fan and distributary channels in the middle fan）,inter-channel,levee-overbank,outer fan and basin microfacies.Facies analysis allows to reconstruct the depositional model of the deepwater fan.During relative sea-level fall,a basin-floor fan formed as sediments from rivers or shelf margin deltas were further transported down slope and into the basin under gravity flows.During the ensuing relative sea-level rise,a slope fan was deposited as the system stepped back.The lower part of the Zhujiang Formation,mainly sandstone-dominated associations,is inner fan and middle-outer fan deposits of the basin-floor and the slope fan respectively.The upper part,mainly mudstone-dominated associations,siltstone associations,and deepwater associations are outer fan deposits of the slope fan and basin deposits.Along with the transgression,submarine fan was finally replaced by pelagic deposits.

关 键 词：珠江口盆地 白云凹陷 荔湾3-1气田 珠江组 深水扇 

分 类 号：P512.2[天文地球—地质学]