莫里青断陷油气运移探究  

A Research on the history of oil and gas migration in Moliqing fault depression

作　　者：余麒麟 孟元林[1] 周新桂[2] 王丹丹[2] 张文浩[2] 张磊[1] 曲国辉[1] 王世磊[1] 

机构地区：[1]东北石油大学地球科学学院,黑龙江大庆163318 [2]中国地质调查局油气资源调查中心,北京100029

出　　处：《中国锰业》2017年第4期41-43,共3页China Manganese Industry

基　　金：国家自然科学基金项目(U1262106;41572135);"十三五"国家科技重大专项(2016ZX05046-001-006);国土资源部中国地质调查局项目(12120115001701);黑龙江省科学基金(QC2016049);黑龙江省普通本科高等学校青年创新人才培养计划(UNPYSCT-2016122);东北石油大学研究生创新科研项目(YJSCX2017-004NEPU)

摘　　要：随着莫里青断陷油气资源的不断开发,为进一步满足高产、稳产的需要,结合莫里青断陷16口井的实测资料,统计分析了72个Ro测试结果、352个(S1+S2)和TOC测试结果,运用生烃潜力法,并结合莫里青断陷复杂而特殊的构造背景,定性并定量地对莫里青断陷油气的初次运移和二次运移时间进行了探讨。结果表明:莫里青断陷双阳组烃源岩在埋深2 400 m±100 m达到排烃门限,开始初次运移,此时与永吉组沉积时期相对应;二次运移大量进行的时期为永吉组和岔路河组沉积时期。With continuous development of oil and gas resources in Moliqing fault depression,we have combined with the measured data of 16 wells in Moliqing fault depression to meet the needs of high yield and stable production. In the meantime,we have analyzed the test results of the vitrinite reflectance,including genetic potential and organic carbon contents in this research. Based on hydrocarbon generation potential method and combined with complex and special tectonic setting of Moliqing fault depression,we have discussed the primary migration and secondary migration time of oil and gas in Moliqing fault depression qualitatively and quantitatively.The results show that the source rocks of Shuangyang Formation in Moriqing fault depression have reached the hydrocarbon expulsion threshold at the depth of 2 400 m ± 100 m. It begins with the primary migration,which corresponds to the sedimentary period of Yongji group. The period of the second migration is a period of time for Yongji Formation and Chaluhe Formation.

关 键 词：莫里青断陷 排烃门限 初次运移 二次运移 

分 类 号：P618.13[天文地球—矿床学]