石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2013年
4期
395-400
,共6页
董才源%刘震%刘启东%罗贝维%李储华%王伟俊
董纔源%劉震%劉啟東%囉貝維%李儲華%王偉俊
동재원%류진%류계동%라패유%리저화%왕위준
断层封闭性%二元主控%成藏体系%断层-岩性油藏%高邮凹陷%苏北盆地
斷層封閉性%二元主控%成藏體繫%斷層-巖性油藏%高郵凹陷%囌北盆地
단층봉폐성%이원주공%성장체계%단층-암성유장%고유요함%소북분지
fault sealing%two controlling factors%accumulation system%fault-lithologic reservoir%Gaoyou Sag%Northern Jiangsu Basin
基于控藏断层封闭性能演化、油藏含油层位和戴南组“五高导”泥岩段生烃能力的差异,高邮凹陷戴南组断层—岩性油藏成藏体系可分为3种类型,依次为自源型、它源型和混源型油气成藏体系。自源型成藏体系主要分布在邵伯、樊川次凹深处,典型油藏为邵深1油藏;它源型油藏主要分布在马家嘴、周22和邵18等油藏区域;混源型油藏以联3、联7和永22等油藏为代表。高邮凹陷戴南组断层—岩性圈闭成藏主要受油源和运移通道控制,即“二元主控”。在成藏体系分布和主控因素分析的基础上,提出黄珏—马家嘴、联盟庄—永安和曹庄—肖刘庄地区是高邮凹陷戴南组断层—岩性油藏分布的最有利区带。
基于控藏斷層封閉性能縯化、油藏含油層位和戴南組“五高導”泥巖段生烴能力的差異,高郵凹陷戴南組斷層—巖性油藏成藏體繫可分為3種類型,依次為自源型、它源型和混源型油氣成藏體繫。自源型成藏體繫主要分佈在邵伯、樊川次凹深處,典型油藏為邵深1油藏;它源型油藏主要分佈在馬傢嘴、週22和邵18等油藏區域;混源型油藏以聯3、聯7和永22等油藏為代錶。高郵凹陷戴南組斷層—巖性圈閉成藏主要受油源和運移通道控製,即“二元主控”。在成藏體繫分佈和主控因素分析的基礎上,提齣黃玨—馬傢嘴、聯盟莊—永安和曹莊—肖劉莊地區是高郵凹陷戴南組斷層—巖性油藏分佈的最有利區帶。
기우공장단층봉폐성능연화、유장함유층위화대남조“오고도”니암단생경능력적차이,고유요함대남조단층—암성유장성장체계가분위3충류형,의차위자원형、타원형화혼원형유기성장체계。자원형성장체계주요분포재소백、번천차요심처,전형유장위소심1유장;타원형유장주요분포재마가취、주22화소18등유장구역;혼원형유장이련3、련7화영22등유장위대표。고유요함대남조단층—암성권폐성장주요수유원화운이통도공제,즉“이원주공”。재성장체계분포화주공인소분석적기출상,제출황각—마가취、련맹장—영안화조장—초류장지구시고유요함대남조단층—암성유장분포적최유리구대。
Based on the studies of fault sealing evolution, oil-bearing formation and hydrocarbon generation ability of highly-conductive mudstones in the Dainan Formation, the fault-lithologic reservoir systems of the Dainan Formation in the Gaoyou Sag have been classified into 3 types, including self-sourced, other-sourced and mixed-sourced. The self-sourced accumulation systems mainly locate in the deep Shaobo and Fanchuan Sags, and the Shaoshen1 resrvoir is typical. The other-sourced accumulation systems mainly distribute in the Majiazui, Zhou22 and Shao18 reservoirs. The mixed-sourced accumulation systems are represented by the Lian3, Lian7 and Yong22 reser-voirs. The fault-lithologic reservoirs of the Dainan Formation in the Gaoyou Sag are controlled by2 elements, oil source and migration pathway. The favorable zones for exploration include Huangjue-Majiazui, Lianmengzhuang-Yongan and Caozhuang-Xiaoliuzhuang.