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鄂尔多斯盆地重力流沉积类型及识别特征OA

Sedimentary types and identification characteristics of gravity flow in Ordos Basin:A case study of Chang-6 oil reservoir of Yanchang Formation in Maling-Qiaochuan area

中文摘要英文摘要

以鄂尔多斯马岭-乔川地区三叠系延长组长6油层组为研究对象,以石油地质学、沉积地层学为理论支撑,对油层组重力流类型、沉积标志、砂体分布特征及沉积模式进行系统解析.基于钻井资料,综合大量岩心及薄片观察,表明砂质碎屑流体为块状构造,内部见漂浮泥质碎屑,浊流以正粒序层理、异重流以沙纹层理为典型识别标志.经进一步细分,确立了浊积中心和边缘微相,并确立"水道-滑塌扇"沉积模式.其中砂质碎屑流成因的厚层块状砂体为有利储集相带,可作为深水区油气勘探的重点层位.

Taking the Chang-6 oil reservoir of Triassic Yanchang Formation in Maling-Qiaochuan area,Ordos Basin,as the research object,supported by petroleum geology and sedimentary stratigraphy,the paper systematically analyzes the gravity flow types,sedimentary marks,sand body distribution characteristics and sedimentary model of oil reservoirs.Based on the drilling data and observation of a large number of cores and thin sections,it is found that the sandy debris flow is in massive structure with floating muddy debris inside.The turbidity current is identified by normal-graded bedding,and density current by ripple bedding.The turbidite center and marginal microfacies,and channel-slump fan sedimentary model are established through further subdivision.The thick massive sand body caused by sandy debris flow is the favorable reservoir facies belt,which can serve as the key horizon for oil and gas exploration in deep water area.

齐诗苇;田亚铭;时孜伟;李继宏;刘志涛

成都理工大学地球科学学院,四川成都 610059||中国石油吉林油田公司勘探开发研究院,吉林松原 138001成都理工大学地球科学学院,四川成都 610059低渗透油气田勘探开发国家工程实验室,陕西西安 710018低渗透油气田勘探开发国家工程实验室,陕西西安 710018成都理工大学地球科学学院,四川成都 610059

天文与地球科学

延长组重力流砂质碎屑流浊积岩沉积模式鄂尔多斯盆地

Yanchang Formationgravity flowsandy debris flowturbiditesedimentary modelOrdos Basin

《地质与资源》 2026 (2)

170-177,8

中国石油天然气股份有限公司长庆油田分公司项目"马岭-乔川地区长6砂体结构及成藏主控因素"(17TD0003).

10.13686/j.cnki.dzyzy.2026.02.005

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