石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2013年
1期
65-71
,共7页
白玉彬%赵靖舟%方朝强%刘鹏
白玉彬%趙靖舟%方朝彊%劉鵬
백옥빈%조정주%방조강%류붕
准连续型油藏%致密砂岩%形成机理%长 6 油层组%鄂尔多斯盆地
準連續型油藏%緻密砂巖%形成機理%長 6 油層組%鄂爾多斯盆地
준련속형유장%치밀사암%형성궤리%장 6 유층조%악이다사분지
quasi-continuous reservoir%tight sandstone%forming mechanism%Chang 6 oil-bearing formation%Ordos Basin
鄂尔多斯盆地陕北斜坡延长组长6油藏为典型的准连续型致密砂岩非常规油藏,主要具有以下7个特点:(1) 长6油藏形成和分布对圈闭无严格要求,石油大面积连片分布,油藏分布范围不受圈闭限制;(2)区域相对稳定的大地构造背景条件,以及大面积复合连片分布的致密储集体是长6准连续型致密砂岩油藏形成的外部因素;(3)长7油层组成熟烃源岩大面积连续分布,高强度生、排烃是长6准连续型致密砂岩油藏形成的前提;(4)长6油藏的形成主要是初次运移和短距离二次运移的结果,垂向裂缝和侧向连通砂体有效组合为石油优势运移通道,石油就近运移聚集成藏;(5)石油运移的动力主要是生烃作用产生的异常压力,浮力作用弱,对油藏的形成和分布不起主要作用;(6)长6油藏油水分布规律复杂,无纯油层,油水层、水层、干层共存,无统一的油水界面和压力系统,油藏非均质性强,含油饱和度不均一,储量丰度较低,存在甜点富集区;(7)在石油大规模生成运移时,长6储层已经致密化或同步致密,为形成长6准连续型致密砂岩油藏创造了条件.
鄂爾多斯盆地陝北斜坡延長組長6油藏為典型的準連續型緻密砂巖非常規油藏,主要具有以下7箇特點:(1) 長6油藏形成和分佈對圈閉無嚴格要求,石油大麵積連片分佈,油藏分佈範圍不受圈閉限製;(2)區域相對穩定的大地構造揹景條件,以及大麵積複閤連片分佈的緻密儲集體是長6準連續型緻密砂巖油藏形成的外部因素;(3)長7油層組成熟烴源巖大麵積連續分佈,高彊度生、排烴是長6準連續型緻密砂巖油藏形成的前提;(4)長6油藏的形成主要是初次運移和短距離二次運移的結果,垂嚮裂縫和側嚮連通砂體有效組閤為石油優勢運移通道,石油就近運移聚集成藏;(5)石油運移的動力主要是生烴作用產生的異常壓力,浮力作用弱,對油藏的形成和分佈不起主要作用;(6)長6油藏油水分佈規律複雜,無純油層,油水層、水層、榦層共存,無統一的油水界麵和壓力繫統,油藏非均質性彊,含油飽和度不均一,儲量豐度較低,存在甜點富集區;(7)在石油大規模生成運移時,長6儲層已經緻密化或同步緻密,為形成長6準連續型緻密砂巖油藏創造瞭條件.
악이다사분지협북사파연장조장6유장위전형적준련속형치밀사암비상규유장,주요구유이하7개특점:(1) 장6유장형성화분포대권폐무엄격요구,석유대면적련편분포,유장분포범위불수권폐한제;(2)구역상대은정적대지구조배경조건,이급대면적복합련편분포적치밀저집체시장6준련속형치밀사암유장형성적외부인소;(3)장7유층조성숙경원암대면적련속분포,고강도생、배경시장6준련속형치밀사암유장형성적전제;(4)장6유장적형성주요시초차운이화단거리이차운이적결과,수향렬봉화측향련통사체유효조합위석유우세운이통도,석유취근운이취집성장;(5)석유운이적동력주요시생경작용산생적이상압력,부력작용약,대유장적형성화분포불기주요작용;(6)장6유장유수분포규률복잡,무순유층,유수층、수층、간층공존,무통일적유수계면화압력계통,유장비균질성강,함유포화도불균일,저량봉도교저,존재첨점부집구;(7)재석유대규모생성운이시,장6저층이경치밀화혹동보치밀,위형성장6준련속형치밀사암유장창조료조건.
The Chang 6 reservoir in the Yanchang Formation in the Shanbei slope of the Ordos Basin is a typical quasi-continuous unconventional tight sandstone reservoir. It has 7 main features as followed. (1) The formation and distribution of the Chang 6 reservoir were not restricted by traps. Oils spread for big area and were connected. (2) Regional relatively stable tectonic background and tight sand bodies connected for big area were the external factors for the formation and distribution of the Chang 6 reservoir. (3) Matured hydrocarbon source rocks in the Chang 7 forma-tion were connected widely. High-strength hydrocarbon generation and expulsion were the basis for the formation and distribution of the Chang 6 reservoir. (4) The Chang 6 reservoir mainly resulted from primary migration and secondary migration of short distance. Vertical cracks and laterally-connected sand body effective combinations provided favora-ble pathways for petroleum migration. (5) The abnormal overpressure caused by hydrocarbon generation was the main force for petroleum migration. Buoyancy effect was very weak and played an unimportant effect in controlling the for-mation and distribution of the reservoir. (6) Oil and water distributions were complex in the Chang 6 reservoir. Pure oil was not found. Oil/ water, water and dry layers coexisted. There was no unified oil/ water boundary or pressure system. The reservoir had strong heterogeneity. Oil saturation was not unified. Reserve abundance was low. Cookies were found locally. (7) The Chang 6 reservoir had been compacted before the mass migration of petroleum, serving foundation for the formation of the Chang 6 quasi-continuous tight sandstone reservoir.