松辽盆地北参1井深层地层划分与对比  

Discussion on Deep Stratigraphic Correlation and Division of Beican-1 Well in Songliao Basin

作　　者：乔秀云[1] 杨建国[1] 孔惠[1] 金玉东[1] 万传彪[1] 

机构地区：[1]大庆油田有限责任公司勘探开发研究院,黑龙江大庆163712

出　　处：《大庆石油地质与开发》2002年第6期13-15,共3页Petroleum Geology & Oilfield Development in Daqing

摘　　要：北参 1井是北安地区目前钻遇下白垩统最全的一口参数井 ,为建立北安地区深层标准剖面以便与松辽盆地深层地层、西北部、东北部的一些外围盆地相关层位进行时代对比 ,采用氢氟酸 -盐酸冷处理方法对 5 2块样品进行处理 ,在 12块岩心样品中获得了孢粉化石。依据古生物岩性资料 ,北参 1井深层 6 0 1 5～ 36 91 0m井段自下而上可划分为 5 1个小层 ,4个组 ,分别为上侏罗统或下白垩统火石岭组、下白垩统沙河子组、营城组和登娄库组。依据北参 1井火石岭组岩性特征提出火石岭组二分的方案。将下部碎屑岩夹煤层划分为火石岭组一段 ,将上部中基性火山岩夹碎屑岩划分为火石岭组二段。火石岭组二分性在松辽盆地北部任 11井、杜 2 2井等许多井均有体现。Beican 1 well is now a best entire parametric well drilling Low Cretaceous in Beian area. In order to establishing the deep stratigraphic key section in Beian area, comparing stratigraphic age between the deep strata in Songliao Basin and the related strata in the peripheral basins of northwest and northeast areas to Songliao Basin, adopting HF HCl cold handling methods to 52 samples, spore and pollen fossils were found in the 12 samples among them. Based on the palaeontologic and lithological data, Beican 1 well hole depth from 601 5 m to 3 691 0 m has been divided into 50 rocks of 4 formations: Huoshiling Formation of Upper Jurassic or Lower Cretaceous,Shahezi Formation,Yengcheng Formation and Denglouku Formation of Lower Cretaceous. Based on lithological characteristics of Huoshiling Formation in Beican 1 well,the Formation is divided into two members: the clastic rocks with interbedded coal in lower part is first member, middle basic volcanic rocks with interbedded clastic rocks in upper part is second member. Existence of two types were proved in Ren11 well and Du22 well in Songliao Basin.

关 键 词：北参1井 地层划分 地层对比 地质时代 孢粉组合 

分 类 号：P618.13[天文地球—矿床学]