沉积与特提斯地质
沉積與特提斯地質
침적여특제사지질
SEDIMENTARY GEOLOGY AND TETHYAN GEOLOGY
2014年
4期
68-74
,共7页
原油地球化学%油源对比%延长组%富县地区%鄂尔多斯盆地
原油地毬化學%油源對比%延長組%富縣地區%鄂爾多斯盆地
원유지구화학%유원대비%연장조%부현지구%악이다사분지
geochemistry of crude oil%oil-source rock correlation%Yanchang Formation%Fuxian region%Ordos Basin
通过对富县地区延长组长6~长9原油及烃源岩的地球化学特征综合对比分析,认为研究区存在长7、长9两套有效烃源岩。长7烃源岩有机质类型为Ⅰ~Ⅱ1型,长9烃源岩的有机类型为Ⅱ1~Ⅱ2型。长7、长9烃源岩中Ts相对含量高于Tm,均达到成熟阶段。长7烃源岩五环三萜烷中C30藿烷丰度相对高于C29藿烷丰度,C30 RH/C29 Ts<2,长7形成于还原环境;长9烃源岩中C30藿烷丰度与C29藿烷丰度基本相似,C30 RH/C29 Ts>2,表明长9为弱氧化-弱还原环境。长6原油饱/芳比值较低,长8原油饱/芳比值较高,说明长6原油和长8原油不同源。长7烃源岩与长9烃源岩在生物标志化合物特征上有明显区别。规则甾烷C27-C28-C29αααR指纹分布样式上,长7呈现“L”型,长9呈现偏“V”型与反“L”型,长8原油呈现偏“V”型分布。研究区长8原油主要来源于长9烃源岩。
通過對富縣地區延長組長6~長9原油及烴源巖的地毬化學特徵綜閤對比分析,認為研究區存在長7、長9兩套有效烴源巖。長7烴源巖有機質類型為Ⅰ~Ⅱ1型,長9烴源巖的有機類型為Ⅱ1~Ⅱ2型。長7、長9烴源巖中Ts相對含量高于Tm,均達到成熟階段。長7烴源巖五環三萜烷中C30藿烷豐度相對高于C29藿烷豐度,C30 RH/C29 Ts<2,長7形成于還原環境;長9烴源巖中C30藿烷豐度與C29藿烷豐度基本相似,C30 RH/C29 Ts>2,錶明長9為弱氧化-弱還原環境。長6原油飽/芳比值較低,長8原油飽/芳比值較高,說明長6原油和長8原油不同源。長7烴源巖與長9烴源巖在生物標誌化閤物特徵上有明顯區彆。規則甾烷C27-C28-C29αααR指紋分佈樣式上,長7呈現“L”型,長9呈現偏“V”型與反“L”型,長8原油呈現偏“V”型分佈。研究區長8原油主要來源于長9烴源巖。
통과대부현지구연장조장6~장9원유급경원암적지구화학특정종합대비분석,인위연구구존재장7、장9량투유효경원암。장7경원암유궤질류형위Ⅰ~Ⅱ1형,장9경원암적유궤류형위Ⅱ1~Ⅱ2형。장7、장9경원암중Ts상대함량고우Tm,균체도성숙계단。장7경원암오배삼첩완중C30곽완봉도상대고우C29곽완봉도,C30 RH/C29 Ts<2,장7형성우환원배경;장9경원암중C30곽완봉도여C29곽완봉도기본상사,C30 RH/C29 Ts>2,표명장9위약양화-약환원배경。장6원유포/방비치교저,장8원유포/방비치교고,설명장6원유화장8원유불동원。장7경원암여장9경원암재생물표지화합물특정상유명현구별。규칙치완C27-C28-C29αααR지문분포양식상,장7정현“L”형,장9정현편“V”형여반“L”형,장8원유정현편“V”형분포。연구구장8원유주요래원우장9경원암。
Geochemical correlation of the crude oil and source rocks from the Chang-8 to the Chang-9 oil reservoirs in the Yanchang Formation,Fuxian region,Ordos Basin indicates that there occur the Chang-7 and Chang-9 effective source rocks with higher organic matter abundances. The organic matter in the Chang-7 source rocks belongs to the I-II1 types,and that in the Chang-9 source rocks belongs to the II1-II2 types,both of which have higher Ts contents than Tm contents,suggesting a mature stage of the source rocks. In the Chang-7 source rocks, C30 hopane abundances in pentacycloterpane are larger than C29 hopane abundances and the C30 RH/ C29 Ts ratios<2,indicating a reduction environment of the Chang-7 source rocks. In the Chang-9 source rocks,a general similarity in C30 hopane abundances and C29 hopane abundances and C30 RH/ C29 Ts ratios>2 indicates the weak oxidation-weak reduction environments of the Chang-9 source rocks. The saturated hydrocarbons/aromatic hydrocarbons ratios are lower in the Chang-6 source rocks than those in the Chang-8 source rocks,indicating different sources of the crude oil from the Chang-6 and Chang-8 source rocks. As for the biomarkers,the C27-C28-C29 αααR distribution patterns of regular steranes in the Chang-7 source rocks display the“L”type,those in the Chang-9 source rocks display the“V”or inverse“L”types,and those in the Chang-8 source rocks display the“V”type. The crude oil in the Chang-8 oil reservoirs mainly stemmed from the Chang-9 source rocks in the study area.