东营凹陷有效烃源岩成熟度评价  

Assessment of the thermal maturity of the effective hydrocarbon source rocks in Dongying Depression

作　　者：张美珍[1] 李志明[1] 秦建中[1] 徐旭辉[2] 施伟军[1] 刘文斌[1] 蒋宏[1] 

机构地区：[1]中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所,江苏无锡214151 [2]中国石油化工股份有限公司石油勘探开发研究院,北京100083

出　　处：《西安石油大学学报（自然科学版）》2008年第3期12-16,共5页Journal of Xi’an Shiyou University（Natural Science Edition）

基　　金：中国石油化工股份有限公司科学技术研究开发项目(编号:P04039)资助

摘　　要：东营凹陷沙三段下亚段-沙四段上亚段有效烃源岩的镜质体反射率存在明显的抑制作用．利用2套有效烃源岩的FAMM分析成果，对其成熟度进行了重新评价．结果表明：烃源岩的有机质类型越好，镜质体反射率抑制程度越强；沙三段下亚段有效烃源岩的真实成熟度一般应在0．56％～1．01％，沙四段上亚段有效烃源岩的真实成熟度一般应在0．58％～1．30％．The vitrinite reflectance value of the effective source rocks of the upper sub-member of the fourth member and the lower sub-member of the third member of Paleogene Shahejie formation (Es) in Dongying Depression is significantly suppressed.The maturity of the two sets effective source rocks is reassessed by means of FAMM (fluorescence alteration of multiple macerals) analysis results.The study shows that the vitrinite reflectance suppression level of the source rocks of organic matter typeⅠranges from 0.24% to 0.35% generally,and that of organic matter type Ⅱ1 and type Ⅱ2 usually ranges from 0.16% to 0.30% and 0.13% to 0.18% respectively.The true thermal maturity of the effective source rocks of the lower sub-member of Es3 and the upper sub-member of Es4 is mainly in 0.56%～1.01% and 0.58%～1.30% separately;but the thermal maturity of them determined by vitrinite reflectance values is in 0.35%～0.80% and 0.37%～1.10% respectively.The study result in this paper has an important role in recognizing the thermal maturity of the source rocks,reevaluating the genesis of oils and the potential of oil resources,and guiding oil and gas exploration.

关 键 词：东营凹陷 有效烃源岩 成熟度 等效镜质体反射率 

分 类 号：TE122.113[石油与天然气工程—油气勘探]