松辽盆地北部泰康—西超地区萨尔图油层岩性油气藏预测
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
大庆油田属于高勘探开发油田,寻找岩性油气藏成了油田增储上产的一个重要途径。根据泰康—西超地区平缓的单斜地质背景,从地质构造特征、烃源岩、沉积特点及油气运移方面分析岩性油气藏的形成条件。区内萨二、三砂组萨一砂组、萨零砂组主要发育砂岩上倾尖灭、地层超覆、砂岩透镜体及复合岩性油气藏,并阐述各类岩性油气藏的形成特征。将沉积微相分布与地震波阻抗反演相结合,预测本区主要岩性油气藏的分布,认为地层超覆岩性油气藏和复合岩性油气藏主要形成于萨二、三砂组,前者主要分布于中西部地区,后者主要分布于阿拉新构造带上,而上倾尖灭、地层超覆、砂岩透镜体岩性油气藏在萨二、三砂组、萨一砂组、萨零砂组都有发育。
Daqing oilfield has been explored in a high degree,so exploring lithology reservoir become a very important way to increase the oilfield reserves.According to Taikang-Xichao area geology setting that is a flat monocline,this thesis studied the petroleum geology condition of forming lithology reservoir based on geology structure character,hydrocarbon source rock,sedimentary character and hydrocarbon migration.In S2+3,S1,S0,upward pinchout,formation onlap,sand lens and combination lithology reservoir are developed,and this study also characterize these different lithology reservoir formation characters.By combining depositional subfacies distribution study and post-seismic impedance inversion study,the main lithology reservoir distribution of this area is predicted,and it is considered that formation onlap lithology reservoir and combination reservoir are mainly developed in S2+3.Onlap lithology reservoir are mainly distributed in the middle and west area,and the combination reservoir is mainly distributed on Alaxin tectonic belt.Upward pinchout,formation onlap,sand lens lithology reservoir are all developed in S2+3,S1,S0.This lithology reservoir study is significant to the future hydrocarbon exploration.
引文
[1]陈启林,杨占龙.岩性油气藏勘探方法与技术[J].天然气地球科学,2006,17(5):623-625.
    [2]翟光明.中国石油地质志(卷二)[M].北京:石油工业出版社,1993:5-147.
    [3]迟元林,蒙启安,杨玉峰.松辽盆地岩性油藏形成背景与成藏条件分析[J].大庆石油地质与开发,2004,23(5):11-14.
    [4]王文广,高宁.西斜坡区萨二、三油层油气成藏机制[J].大庆石油学院学报,2006,30(1):2-5.
    [5]付晓飞,王朋岩,申家年,等.简单斜坡油气富集规律——以松辽盆地西部斜坡北段为例[J].地质评论,2006,52(4):524-527.
    [6]邹才能,薛叔浩,赵文智,等.松辽盆地南部白垩系泉头组—嫩江组沉积层序特征与地层—岩性油气藏形成条件[J].石油勘探与开发,2004,31(2):16-20.
    [7]张维琴,杨玉峰.松辽盆地西部斜坡油气来源与运移研究[J].大庆石油地质与开发,2005,24(1):18-23.
    [8]赵荣,梅丽,陈峰,等.西斜坡区油型气成藏与分布的主控因素及有利勘探区预测[J].大庆石油学院学报,2006,30(6):6-11.
    [9]孙英杰,付广,张然.松辽盆地北部源岩和盖层的时空匹配关系及其对天然气聚集与分布的控制[J].现代地质,2003,17(3):321-328.
    [10]江涛,苗洪波,王芳,等.松辽盆地西部盆缘带地层超覆油藏形成条件[J].大庆石油地质与开发,2006,25(4):25-28.
    [11]蒙启安,杨永斌,金明玉.断裂对松辽盆地庆深大气田的控制作用[J].石油学报,2006,27(增刊):16-19.
    [12]向才富,夏斌,解习农,等.松辽盆地西部斜坡带油气运移主输导通道[J].石油与天然气地质,2004,25(2):206-207.
    [13]周庆华,吕延防,汪松,等.松辽盆地敖古拉断裂带的封闭性及其对西斜坡油气运聚的控制作用研究[J].天然气地球科学,2008,19(2):214-215.
    [14]蒙启安,黄薇,林铁峰,等.松辽盆地北部岩性油藏形成条件与分布规律[J].中国石油勘探,2004(4):9-12.
    [15]周庆华,吕延防,付广,等.松辽盆地北部西斜坡油气成藏模式和主控因素[J].天然气地球科学,2006,17(6):766-769.
    [16]杨玉峰.松辽盆地岩性油藏形成条件与分布规律[J].石油与天然气地质,2004,25(4):499-504.
    [17]邹才能,陶士振,谷志东.陆相坳陷盆地层序地层格架下岩性地层圈闭/油藏类型与分布规律——以松辽盆地白垩系泉头组—嫩江组为例[J].地质科学,2006,41(4):713-716.
    [18]杨玉峰,杨波.松辽盆地北部西部超覆带稠油形成机理与分布规律研究[R].大庆:大庆油田勘探开发研究院,2002:34-36.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心