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梅河盆地沉积体系及沉积体系域
引用本文:胡善亭,荆惠林.梅河盆地沉积体系及沉积体系域[J].煤田地质与勘探,1996,24(3):4-8.
作者姓名:胡善亭  荆惠林
作者单位:中南工业大学,长春煤田地质研究所
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。

关 键 词:盆地,沉积环境,演化,吉林

THE DEPOSITIONAL SYSTEMS AND DEPOSITIONAL SYSTEM TRACTS IN MEIHE BASIN
Hu Shaming.THE DEPOSITIONAL SYSTEMS AND DEPOSITIONAL SYSTEM TRACTS IN MEIHE BASIN[J].Coal Geology & Exploration,1996,24(3):4-8.
Authors:Hu Shaming
Institution:Hu Shaming (Central South University of Technology)Jing Hueilin;Wu Keping;Wang Liwei(Changchun Institute of Coal Geology)
Abstract:eihe basin is the constitution southern sector of the great Fushun-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 system 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.
Keywords:asin  depositional environment  evolution  jilin  
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