渤海湾盆地潍北凹陷孔三段火山溢流相旋回与期次划分  

Cycles and stages division of volcanic effusive phase of the third member of Kongdian Formation in Weibei Sag,Bohaiwan Basin

作　　者：孙耀庭 徐守余[1] 买买提吐尔逊.库吐鲁 郭玉新 赵约翰[2] 刘静[2] SUN Yaoting;XU Shouyu;MMTTUERXUN Kultulu;GUO Yuxin;ZHAO Yuehan;LIU Jing(School of Geosciences in China University of Petroleum,Qingdao 266580,China;Geo-Science Research Institute,Shengli Oilfield Company,SINOPEC,Dongying 257015,China;Karamay Mud Logging Engineering Company of XDEC Limited,CNPC,Karamay 834000,China)

机构地区：[1]中国石油大学地球科学与技术学院,山东青岛266580 [2]中国石化胜利油田分公司勘探开发研究院,山东东营257015 [3]中国石油西部钻探工程有限公司克拉玛依录井工程公司,新疆克拉玛依834000

出　　处：《中国石油大学学报（自然科学版）》2018年第2期29-40,共12页Journal of China University of Petroleum(Edition of Natural Science)

基　　金：国家科技重大专项(2011ZX05006)

摘　　要：潍北凹陷孔三段广泛发育火山岩地层,有效储层主要发育在溢流相。综合利用岩心、测井、地震资料对火山溢流相的旋回和期次进行划分,研究表明:潍北凹陷孔三段火山岩可划分为2个喷发旋回7个期次,每期火山溢流相熔岩层垂向可划分为上部、中部和下部3个亚相,其中上部亚相气孔和杏仁构造最为发育,是火山岩最优质的储层类型;依据火山岩熔岩流规模变化可将溢流相划分为Ⅰ型熔岩层系(扩张型)和Ⅱ型熔岩层系(收缩型)2种类型,Ⅰ型熔岩层系有利储层分布在层系上部,Ⅱ型熔岩层系有利储层分布在层系下部;Ⅰ型熔岩层系在喷发早期(4~7期)发育,规模较大,Ⅱ型熔岩层系在喷发晚期(1~3期)发育,规模较小,反映了火山早期活动强烈,晚期逐步减弱的发育过程。The volcanic strata w-ere widely developed in the 3rd member of Kongdian Formation of Weibei Sag,w-here the effective reservoirs were mainly developed in effusive phases.Eruption cycles and stages of the effusive phases were categorized comprehensively using cores,logging and seismic data.The results show-that volcanic rocks can be divided into two eruptive cycles and seven eruptive stages.Each eruptive cycle can be vertically divided into three subfacies:the upper subface,the central subfaces and the lower subface,respectively.Air holes and almond constructions were developed in the upper subface,which is the best reservoir type of volcanic rocks.According to the scale of lava flows,effusive phases are divided into two types,progradational and retrogradational cycles.Favorable reservoirs are mainly distributed in the upper part of the progradational layers,and the lower part of the retrogradational layers.Progradational layers have larger scales,developed during the early eruption(from4th to 7th)stages;w-hile retrogradational layers have smaller scales,developed during later eruption(from 1st to 3rd)stages.It is suggested that early volcanic activities were intensive,which were gradually w-eakened through time.

关 键 词：火山岩 溢流相 喷发旋回 期次 潍北凹陷 渤海湾盆地 

分 类 号：P618.130.2[天文地球—矿床学]