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中国东北地区与白俄罗斯全新世成炭期对比及成因分析

Comparison of Peatification Periods of Holocene in the Northeast of China and in Byelorussia and Analyses of Its Formation Cause

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【Author】 Leng Xuetian Li Yiyin (Department of Geography, Northeast Normal University,Changchun,130024,China) S.G.Bellinge (Institute for Problems of Natural Resources Use & Ecology,Academy of Sciences of Belarus,Minsk,220114,Byelorussia)

【机构】东北师范大学地理系；

【摘要】通过两地成炭期对比，分析其成炭气候差异和原因，揭示出影响两地成炭作用的气候机制，进而探讨了北方湿润气候带的全新世变迁更多还原

【Abstract】 Because the northern moist climatic zone has ever moved or swayed along meridian in the geological periods, the peatification belts also change with it. It analyses the climatic difference of peatification of the two areas and discuss the change orits of the belt in Holocene and advance its trends in future through contrasting the peatification periods of the two areas.更多还原

【关键词】泥炭；全新世；成炭期；北方湿润气候带；
【Key words】 peat； holocene； peatification period； northern moist climatic zone；

【基金】国家自然科学基金资助的国际合作项目

【文献出处】东北师大学报(自然科学版) ,JOURNAL OF NORTHEAST NORMAL UNIVERSITY (NATURAL SCIENCE EDITION) , 编辑部邮箱 ,1997年01期

【分类号】P611
【被引频次】6
【下载频次】96

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