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作 者:王亚青[1] 林承焰[1] 董春梅[1] 邢焕清[2]
机构地区:[1]中国石油大学(华东)地球资源与信息学院,山东东营257061 [2]胜利油田有限公司地质科学研究院,山东东营257015
出 处:《西安石油大学学报(自然科学版)》2008年第2期16-19,23,共5页Journal of Xi’an Shiyou University(Natural Science Edition)
摘 要:以东营凹陷中央隆起带西段史115深水浊积扇岩性油藏为例,对储层非均质性的时空演变规律及主要控制要素进行研究,认为构造运动、湖平面变化、沉积物供给和古地貌等要素控制了扇体的发育,从而导致储层非均质性在不同时间和空间里表现出明显的差异.浊积扇发育早期,构造运动和古地貌造成扇体规模较小,储层非均质性最强.浊积扇发育中期,构造运动减弱和填平补齐作用导致扇体分布范围增大,储层非均质性较强.浊积扇发育晚期,随着构造运动进一步减弱、湖平面下降,扇体平面分布范围更加广泛,储层非均质性最弱.The study on the characterization of reservoir heterogeneity should be from static state to dynamic state.Taking the Shi-115 block located in the west of central uplift belt of Dongying Sag as an example,the space-time evolution law and controlling factors of the heterogeneity of the deepwater turbidite fan reservoir are studied.It is held that,tectonic movement,lake-level fluctuation,the supply rate of sediments and palaeogeomorphology control the development of the turbidite fan,and therefore there is significant difference in the reservoir heterogeneity in different space and time.In the early stage of the fan development,tectonic movement and palaeogeomorphology result in the small distribution range of the turbidite fan,and the heterogeneity of the reservoir is the severest.In the middle stage,the distribution range of the turbidite fan expands due to the weakening of the tectonic movement and the backfill of sediment,and therefore the heterogeneity of the reservoir becomes slightly weaker.In the late stage,with the further weakening of the tectonic movement and the descending of lake-level,the distribution range of the turbidite fan further expands,and the heterogeneity of the reservoir is the weakest.
关 键 词:东营凹陷 储层非均质性 主控要素 构造运动 湖平面升降 沉积物供给
分 类 号:TE122.2[石油与天然气工程—油气勘探]
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