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四川筠连矿区蒿坝矿段沉积环境及聚煤规律浅析
引用本文:朱敏杰,王海清.四川筠连矿区蒿坝矿段沉积环境及聚煤规律浅析[J].四川地质学报,2011,31(2):149-152.
作者姓名:朱敏杰  王海清
作者单位:四川华源矿业勘查开发有限责任公司,成都,610072
摘    要:通过对区内岩性、沉积构造、古生物、地球化学特征以及对区内沉积相、沉积旋回、沉积模式等沉积环境的初步分析,认为研究区含煤建造形成于潮坪~泻湖沉积体系,由湖泊相、泻湖相、潮坪相、泥炭沼泽相组成.区内稳定可采的主要煤层形成于岛后潮坪~泻湖演变成的泥炭沼泽,厚度大,延伸广.影响区内各煤层厚度和煤质变化的沉积因素主要有地形、蓄水盆地水位、海相顶板等.

关 键 词:煤矿  沉积环境  聚煤规律  筠连

Sedimentary Environment and Coal-Accumulating Patterns in the Songba Ore Block, Junlian Coal Mine, Sichuan
ZHU Min-jie,WANG Hai-qing.Sedimentary Environment and Coal-Accumulating Patterns in the Songba Ore Block, Junlian Coal Mine, Sichuan[J].Acta Geologica Sichuan,2011,31(2):149-152.
Authors:ZHU Min-jie  WANG Hai-qing
Institution:(Huayuan Mineral Exploration and Development Company Limited,Chengdu 610072)
Abstract:Study of lithologic character,sedimentary structure,paleontology and geochemistry as well as sedimentary facies,sedimentary circulation and sedimentary model indicates that the coal-bearing formation in the Songba ore block,Junlian coal mine was formed in tidal flat-lagoon depositional system and consists of lacustrine facies,lagoon facies,tidal flat facies and peat moor facies.Major mineable seams were formed in back barrier peat moor facies.Change in thickness and quality of coal beds is controlled by topography,water level and marine roof.
Keywords:coal mine  sedimentary environment  coal-accumulating pattern  Junlian
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