鄂尔多斯盆地重力流沉积类型及识别特征——以马岭-乔川地区延长组长6段油层组为例

    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

    • 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.

       

      Abstract: 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.

       

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