摘要
陕北斜坡中部杏子川油田延长组原油物性、族组成、饱和烃气相色谱、萜甾烷生物标志化合物以及地质综合分析显示,不同层位延长组原油地球化学特征具有显著的差异。长4+5、长6原油性质基本一致,具有同源属性,其差异性可能主要与运移分馏效应以及原油成熟度有关。长9、长10原油与长4+5、长6原油性质具有明显的差异,反映了其具有不同的母源属性。Ts/Tm、C29ββ/(ββ+αα)、αααC2920S/(20S+20R)等反映原油成熟度的生物标志化合物显示长9、长10原油具有较高的成熟度。长9和长10原油规则甾烷含量显示具有不同的成因。地质综合分析和油源对比表明:长4+5、长6原油均来自于长7生油岩,长9原油来自于其顶部的李家畔页岩,长10原油可能主要来源于长92有效烃源岩。
There are significant differences between the crude oil in different horizons of Yanchang Formation, as is shown by the property, group composition, gas chromatography of saturated hydrocarbon, biomarker of terpane and sterane, comprehensive geological analyses. The crude oil properties of Chang-4＋5 and Chang-6 are gener- ally consistent and isogenous, whose difference may be related to migration fractionation effect and crude oil ma- turity. However, there exist obvious variances in the crude oil property between Chang-9 or Chang-10 and Chang-4＋5 or Chang-6, indicating different maternal properties. The crude oils in Chang-9 and Chang-10 have relatively higher maturity, mirrored by the biomarkers of Ts/Tm, C29ββ/（ββ＋αα） 20R）, etc. The content of regular sterane in the crude oils in Chang-9 and Chang-10 Thus, 5 and and αααC2920S/ （ 20S ＋ shows different genesis. the comprehensive geological analyses and oil-source correlation manifest that the crude oils in Chang-4＋ Chang 6 come from the source rocks of Chang-7, while the crude oils in Chang-9 generate from the Lijia- pan shale, and the crude oils in Chang-10 may stem from the effective source rocks of Chang-92.
出处
《石油实验地质》
CAS
CSCD
北大核心
2013年第5期552-558,共7页
Petroleum Geology & Experiment
基金
陕西省教育厅专项科研计划项目(12JK0491)
陕西省自然科学基础研究计划资助项目(2013JM5007)
中国石油科技创新基金项目(2011D-5006-0103)资助
关键词
原油地球化学
油源对比
延长组
杏子川油田
鄂尔多斯盆地
crude oil geochemistry
oil-source correlation
Yanchang Formation
Xingzichuan Oiliield
Ordos Basin
