中国材料进展
中國材料進展
중국재료진전
Materials China
2015年
10期
719-725
,共7页
杜凌春%李凤杰%屈雪林%张雁%侯景涛%苏幽雅
杜凌春%李鳳傑%屈雪林%張雁%侯景濤%囌幽雅
두릉춘%리봉걸%굴설림%장안%후경도%소유아
残余地层%油藏控制因素%长 2 油层组%吴起地区%鄂尔多斯盆地
殘餘地層%油藏控製因素%長 2 油層組%吳起地區%鄂爾多斯盆地
잔여지층%유장공제인소%장 2 유층조%오기지구%악이다사분지
Paleogeomorphy%oil pool%controlling factor%Chang 2 oil reservoir group%Wuqi area%Ordos Basin
通过铸体薄片、扫描电镜和压汞分析,以及依据油藏所处的构造形态、储层成因类型、油藏成藏要素等对油藏进行解剖分析,探讨鄂尔多斯盆地吴起地区长2油层组侵蚀残余地层油藏的控制因素。吴起地区长2油层组储层砂体孔隙类型主要为剩余原生粒间孔和次生溶孔,孔隙结构分选中等;发育上倾尖灭型、透镜体型、小幅背斜构造型和复合成因型4种油藏类型。鄂尔多斯盆地延长组侵蚀残余地层油藏成藏受古地貌、岩性和构造等多重因素的控制,油藏主要分布于古河道两侧的斜坡带上。地层完整的长2油层组内,小幅背斜构造与分流河道砂体叠置,形成规模较大的构造-岩性复合成因油藏,是吴起地区长2油层组主要的油藏类型。
通過鑄體薄片、掃描電鏡和壓汞分析,以及依據油藏所處的構造形態、儲層成因類型、油藏成藏要素等對油藏進行解剖分析,探討鄂爾多斯盆地吳起地區長2油層組侵蝕殘餘地層油藏的控製因素。吳起地區長2油層組儲層砂體孔隙類型主要為剩餘原生粒間孔和次生溶孔,孔隙結構分選中等;髮育上傾尖滅型、透鏡體型、小幅揹斜構造型和複閤成因型4種油藏類型。鄂爾多斯盆地延長組侵蝕殘餘地層油藏成藏受古地貌、巖性和構造等多重因素的控製,油藏主要分佈于古河道兩側的斜坡帶上。地層完整的長2油層組內,小幅揹斜構造與分流河道砂體疊置,形成規模較大的構造-巖性複閤成因油藏,是吳起地區長2油層組主要的油藏類型。
통과주체박편、소묘전경화압홍분석,이급의거유장소처적구조형태、저층성인류형、유장성장요소등대유장진행해부분석,탐토악이다사분지오기지구장2유층조침식잔여지층유장적공제인소。오기지구장2유층조저층사체공극류형주요위잉여원생립간공화차생용공,공극결구분선중등;발육상경첨멸형、투경체형、소폭배사구조형화복합성인형4충유장류형。악이다사분지연장조침식잔여지층유장성장수고지모、암성화구조등다중인소적공제,유장주요분포우고하도량측적사파대상。지층완정적장2유층조내,소폭배사구조여분류하도사체첩치,형성규모교대적구조-암성복합성인유장,시오기지구장2유층조주요적유장류형。
This paper analyses the casting thin sections,scanning electron microscope and mercury injection.The result shows that the rock types of the Chang 2 (Member 2 of Triassic Yanchang Formation)oil reservoir group in the Wuqi area of Ordos Basin are mainly the fine-grain feldspathic lithic sandstone and lithic arkose,the types of reservoir space are mainly the residual original intergranular pores and the secondary solution pores,and the sorting reservoir pore structure is medium.Based on the detailed analysis of the reservoir structure in paleogeomorphology,the genetic types of the reservoir,and the reservoir accumulation elements,etc.,4 types of oil reservoirs,that is,the updip pinch-out type,the lens shape,the small anticline structure type and the compound genesis type,develop in the Chang 2 oil layer group of the Wuqi area.It can be concluded that the Yanchang Formation erosion residual geomorphology reservoir in Ordos Basin is controlled by multiple factors,such as,geomorphology,lithology and structure.The reservoir is mainly distributed over the <br> river on both sides of the slope.In the Chang 2 oil layer group with complete formation,the anticline structure is slightly superimposed on the distributary channel sandstone.There develop a larger composite genetic oil pool of structure and lithology.It is the main oil pool type in the Chang 2 oil layer group of the Wuqi area.