鹤岗盆地含煤岩系沉积体系及沉积环境分析  

Analysis of Sedimentary System and Sedimentary Environment of Coal Bearing Strata in Hegang Basin

作　　者：张金彪 李柱[2] 

机构地区：[1]黑龙江省煤田地质勘察设计研究院,哈尔滨150008 [2]中国矿业大学,北京100083

出　　处：《煤炭技术》2014年第4期86-89,共4页Coal Technology

摘　　要：通过沉积相分析,确定了鹤岗盆地为陆相断陷湖盆沉积的冲积扇—辨状河—曲流湖—湖泊三角洲—湖泊沉积体系。通过连井剖面着重分析了沉积相垂向及平面的分布特征,对鹤岗盆地成煤时期沉积环境有了初步的了解。Through analysis of sedimentary facies,the Hegang basin is a continental rift basin alluvial fan-braided and meander Lake-lake delta lacustrine depositional system.By connecting well section focuses on the analysis of the distribution characteristics of sedimentary faces in vertical and plane of Hegang basin,the sedimentary environment of coal period had the preliminary understanding.

关 键 词：鹤岗盆地 沉积相 沉积体系 沉积环境 

分 类 号：P618[天文地球—矿床学]