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塔里木盆地巴楚中奥陶统一间房组生物礁-滩发育模式和储集物性 被引量:3

Reef-shoal depositional model and reservoir qualities of middle Ordocician Yijianfang formation in Bachu,Tarim Basin
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摘要 依据精细的露头写实及室内分析,对塔里木盆地巴楚一间房露头区中奥陶统一间房组生物礁-滩沉积体系发育模式及储集性能进行研究。结果表明:一间房组自下而上共划分为5个三级层序,每个层序均由TST和HST构成,生物礁-滩沉积体系主要发育于层序1至层序3中,由生物礁、生物碎屑滩和台缘背景沉积3种成因相组合构成;层序1和层序2的HST内发育进积型生物礁-滩沉积体系,以沉积高能带向盆地方向迁移为特点;层序3的TST内发育退积型生物礁-滩沉积体系,以沉积高能带向台地方向迁移为特点,其中早期为海侵追补型,晚期为海侵并进型;在生物礁-滩沉积体系中,礁前内侧砂质滩和礁后内侧砂质滩具有相对较好的储集性能,是潜在的优质储层。 Fine outcrop description as well as laboratory analysis were carried out to reveal the depositional model and the features of reservoir quality distribution of platform margin reef-shoal depositional system of the middle Ordocician Yijiangfang formation in Bachu Yijiangfang outcrop.The results show that Yijianfang formation is divided into five three-order sequences from bottom to top,each of which is comprised of TST and HST.Formed by three genetic facies namely reef,bioclastic beach and background deposit of platform,the reef-shoal depositional system mainly develops at the carbonate platform margins of sequence 1 to sequence 3.The prograding reef-shoal depositional system is featured by the movement of high energy zone towards basin direction,and developed in the HST of sequence 1 and sequence 2.In the TST of sequence 3,the retrograding reef-shoal depositional system is developed with the constant moving of high energy zone to the platform.In such a sequence,catch-up transgression reef-shoal complex develops in the early period,whereas keep-up transgression reef-shoal complex grows in the later one.In the reef-shoal depositional system,the reef-front interior arenaceous beaches and reef-back interior arenaceous beaches are usually potentially high-quality reservoirs.
出处 《中国石油大学学报(自然科学版)》 EI CAS CSCD 北大核心 2012年第1期47-52,59,共7页 Journal of China University of Petroleum(Edition of Natural Science)
基金 中国石油化工集团公司前瞻性项目(YPH08114)
关键词 塔里木盆地 巴楚地区 一间房组 生物礁-滩 沉积模式 储集物性 Tarim Basin Bachu area Yijianfang formation reef-shoal depositional model reservoir qualities
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