塔里木盆地北部三叠-侏罗纪物源区板块构造背景与沉积盆地类型关系的研究

1996年 18卷 第3期
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PLATE STRUCTURAL SETTING OF THETRIASSIC-JURASSIC PROVENANCE AND ITSRELATIONSHIP WITH SEDIMENTARY BASIN TYPEIN THE NORTH OF THE TARIM BASIN
张希明 刘青芳 王贵全
Zhang Ximing Liu Qingfang Wang Guiquan
西北石油地质综合研究大队, 乌鲁木齐830011
Comprehensive Research Party, Northwest Bureau of Petroleum Geology
作者通过对大量地表和钻井剖面砂岩薄片的系统观察研究,认为本区北部的库车拗陷属前陆盆地;南部的阿瓦提-满加尔拗陷为克拉通内拗陷盆地。在盆地类型分析的基础上,结合本区油气勘探的成果,对盆地油气藏分布模式和油气资源勘探远景进行了分析、预测。
In the light of systematic study of a large number of sandstone thin-sections from surface exposure and wells, the authors considered that the Kuqa depression in the north ofthe Tarim basin was a foreland basin,and the Awat-Mannaer depression was an intra cratonic downwarped basin. On the basis of analysis of basinal types,combining the result ofoil/gas exploration in the area,the distribution pattern of hydrocarbon accumulation andhydrocarbon exploration prospect were analysed and predicted.
塔里木盆地北部; 碎屑组分; 物源区类型; 板块构造背景; 沉积盆地;
https://doi.org/10.11781/sysydz199603252