琼东南盆地崖城组聚煤环境及成煤规律  

The Coal-Accumulating Environment and Coal-Forming Model of Yacheng Formation in Qiongdongnan Basin

作　　者：任桂媛[1,2] 肖军[1] 李彦丽[1] 廖计华[1] 李国良 夏存银 

机构地区：[1]中国地质大学资源学院,武汉430074 [2]中国石油南方石油勘探开发有限责任公司,广州510240 [3]中海石油天津分公司,天津300452

出　　处：《新疆石油地质》2011年第6期621-623,共3页Xinjiang Petroleum Geology

基　　金：国家自然科学基金项目(40702023);国家科技重大专项(2008ZX05023-04-006)

摘　　要：综合利用钻井、岩心及地震等资料,结合沉积学及层序地层学相关方法和理论,对琼东南盆地崖城组聚煤环境特征及成煤作用展开研究。琼东南盆地崖城组煤层主要见于潮坪潮上带和潮间带的泥炭坪、辫状河三角洲平原泥炭沼泽及扇三角洲平原泥炭沼泽。以聚煤环境为主线,考虑到古构造的影响,总结出琼东南盆地的聚煤模式:潮上带及潮间带面积最大,为主要的聚煤环境;缓坡带成煤沉积体系的分布广于断控陡坡带;崖二段具有较强的聚煤潜力。Based on the drilling data,core data and seismic information,this paper discusses about features of coal-accumulating environment and coal-forming of Yacheng formation in Qiongdongnan basin with application of methods and theories of sequence stratigraphy and sedimentology.Coal seams of the Yacheng formation are mainly found in peat flat of supralittoral zone and intertidal zone of tidal flat,peat swamps of the braided river delta plain and fan-delta plain.Focusing on the coal-accumulating environment and considering the influence of paleostructure,the coal-accumulating model for Qiongdongnan basin is developed as following： the supralittoral zone and intertidal zone in tidal flat are of the largest area,being the main coal-accumulating environment;the distribution of coal-forming sedimentary system in gentle slope zones is broader than that in steep slope zones controlled by faults;the second member of Yacheng formation is of greater potentiality of coal-accumulating.

关 键 词：琼东南盆地 崖城组 聚煤环境特征 成煤规律 

分 类 号：P618.1[天文地球—矿床学]