梅河盆地沉积体系及沉积体系域
THE DEPOSITIONAL SYSTEMS AND DEPOSITIONAL SYSTEM TRACTS IN MEIHE BASIN
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摘要: 梅河盆地是抚顺——密山深大断裂南段的组成部分,是一个典型的断陷型聚煤盆地。根据钻探、测井和粒度分析等资料,对沉积体系和沉积体系域进行了分析,梅河盆地主要沉积体系有冲积扇-扇三角洲沉积体系、湖泊沉积体系和河流-三角洲沉积体系,每一种沉积体系都由一套有规律的沉积组合构成。随着盆地的演化,梅河盆地先后出现了冲积扇-辫状河、冲积扇-扇三角洲-湖泊、河流-三角洲一湖泊等沉积体系域。Abstract: Meihe basin is the constitution southern sector of the great Fushun一Mishan deep fault.It is a typical coal-accumulating fault basim.The depositional systems and depositional system tracts are studied with real core,logging and grain size analysis etc.The main depositional systems are alluvial fan-fan-delta depositional system,lacustrine depositional system and fluvial-delta depositional system.Every depositional bystem consists of a serial sedimentary units.The alluvial fan-braided stream dapositional system tract,the alluvial fan-fan-detal-lacustrine depositional system tract and fluvial-detal-lacustrine depositional system tract are occurred in different evolutionary stage of basin.