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柴达木盆地南翼山构造油砂山组混积沉积相特征
引用本文:罗芳,牟中海,罗晓兰,赵振伟.柴达木盆地南翼山构造油砂山组混积沉积相特征[J].石油地质与工程,2009,23(6):5-8,11.
作者姓名:罗芳  牟中海  罗晓兰  赵振伟
作者单位:1. 西南石油大学,四川成都,610500
2. 中国石油青海油田公司勘探开发研究院
3. 中国石油川庆钻探工程有限公司地球物理公司
摘    要:南翼山构造位于青海省柴达木盆地西部北区,属于西部坳陷区茫崖凹陷南翼山背斜带上的一个三级构造。通过对取心资料和录井资料统计,工区目的层为以碳酸盐岩为主的碳酸盐岩与砂岩的混积咸水半深湖相加浅湖相沉积。对剖面沉积相、沉积相相序等进行了分析,同时对主要含油小层进行了平面沉积微相展布研究,在此基础上,结合区域地质资料,并以相递变律为理论依据,总结出了南翼山油砂山组沉积相特征。

关 键 词:柴达木盆地  南翼山构造  混积  湖相  沉积相

Mixed sedimentary fades of Youshashan formation in Nanyishan structure of Qaidam basin
Abstract:Nanyishan structure,located in the north of the western Qaidam basin in Qinghai province,belongs to a third-level structure in the western Mangya depression area of Nanyis-han anticline belt.After coring and mud logging analysis,the target layer is found to be in a mixed sedimentary facies,mainly composed by carbonate and sandstone.Through anal ysis and research of profile sedimentary characteristics,faci es sequence,and microfacies distribution of main oil-bear ing layers,in combination with geologic data and on the ba sis of facies sequence grading rules,the sedimentary facies characteristics of Youshashan formation in Nanyishan struc ture of Qaidam basin has been summarized in this paper.
Keywords:Qaidam basin  Nanyishan structure  diamictite  lake facies  sedimentary facies
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