新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2013年
2期
199-201
,共3页
张亮%曾昌民%黄智斌%陈才%朱礼春%沈春光%吕惠贤
張亮%曾昌民%黃智斌%陳纔%硃禮春%瀋春光%呂惠賢
장량%증창민%황지빈%진재%주례춘%침춘광%려혜현
西南坳陷%柯东1号构造%白垩系%地化特征%混合原油
西南坳陷%柯東1號構造%白堊繫%地化特徵%混閤原油
서남요함%가동1호구조%백성계%지화특정%혼합원유
Southwest depression%No.1 KeDong structure%Cretaceous%Geochemical characteristics%Crude Oil
柯东1号构造是塔里木盆地西南坳陷昆仑山前发育的断鼻型圈闭,钻探kd1井白垩系获高产工业油气流.原油地球化学特征表明,其为高含蜡中质成熟原油,甾烷中C27、C28、C29甾烷呈反“L”型分布,以C29甾烷含量高为特征,萜烷类C29、C30重排霍烷、C30未知萜烷、C24四环萜烷、Ts含量相对较高.生物标志物特征表明,该原油来源于二叠系烃源岩.据原油成熟度分析认为,该原油高分子量芳烃和低分子量的轻烃是烃源岩分别在成熟阶段与高-过熟阶段产物.因此,kd1井白垩系原油是二叠系烃源岩成熟期、高熟期两期充注的混合原油.
柯東1號構造是塔裏木盆地西南坳陷昆崙山前髮育的斷鼻型圈閉,鑽探kd1井白堊繫穫高產工業油氣流.原油地毬化學特徵錶明,其為高含蠟中質成熟原油,甾烷中C27、C28、C29甾烷呈反“L”型分佈,以C29甾烷含量高為特徵,萜烷類C29、C30重排霍烷、C30未知萜烷、C24四環萜烷、Ts含量相對較高.生物標誌物特徵錶明,該原油來源于二疊繫烴源巖.據原油成熟度分析認為,該原油高分子量芳烴和低分子量的輕烴是烴源巖分彆在成熟階段與高-過熟階段產物.因此,kd1井白堊繫原油是二疊繫烴源巖成熟期、高熟期兩期充註的混閤原油.
가동1호구조시탑리목분지서남요함곤륜산전발육적단비형권폐,찬탐kd1정백성계획고산공업유기류.원유지구화학특정표명,기위고함사중질성숙원유,치완중C27、C28、C29치완정반“L”형분포,이C29치완함량고위특정,첩완류C29、C30중배곽완、C30미지첩완、C24사배첩완、Ts함량상대교고.생물표지물특정표명,해원유래원우이첩계경원암.거원유성숙도분석인위,해원유고분자량방경화저분자량적경경시경원암분별재성숙계단여고-과숙계단산물.인차,kd1정백성계원유시이첩계경원암성숙기、고숙기량기충주적혼합원유.
No.1 KeDong structure is an anticline like broken nose develops at the Kunlun piedmont in the southwest de-pression of the Tarim basin.Kd1 well drilling in the Cretaceous got a high yield. The geochemical characteristics of Crude oil show that the oil is medium maturity oil including high wax.The sterane pattern of C27,C28 and C29 is re-versed“L”,the content of C29 is high value.The C30 unknown terpene,C24 ethynylation and the Ts/Tm has high value. The characteristics of biological markers show that the crude oil should come from Permian hydrocarbon source rocks. Maturity analysis suggest that low molecular weight hydrocarbons are producted in high-over ripe stage,and the high mo-lecular weight hydrocarbons maturity parameters indicated that when the oil formed,hydrocarbon source rocks are at high-over ripe stage.Therefore,we think that kd1 crude oil is mixed from Permian hydrocarbon source rocks mature peri-od, high ripe stage.