内蒙古呼伦贝尔地区地质构造的基本特征

Basic characteristics of geological structure in Hulun Buir area, Inner Mongolia

内蒙古呼伦贝尔市是全中国乃至全世界的最大土地管辖面积区级城市,呼伦贝尔的草原也享有世界上最好的草原此美誉称号,呼伦贝尔地处中俄蒙三国的交接地带,不同的地质条件与特征所构成的经济类型也不同,以大兴安岭为分界线,岭西是呼伦贝尔大草原,岭东多为平原与丘陵,在草原与山地的过渡地段多是黑钙土。研究地区地质构造特征是了解一个城市历史发展与未来展望的有效举措,本文就内蒙古呼伦贝尔地区地质构造基本特征进行探讨。

Inner Mongolia is the largest city in Hulun Buir and even the whole world all the land Chinese area under the jurisdiction of district level city,the grasslands of Hulun Buir also enjoy the world＇s best grassland this reputation title,Hulun Buir is located in the Sino Russian Mongolia transfer zone,which is different to different geological conditions and characteristics of the economic type,taking Greater Khingan Range as the dividing line.The west is the Hulun Buir prairie,is plain and hilly region,grassland and mountains in the transition section is chernozem.The study of regional geological structure is an effective measure to understand the historical development and future prospects of the city,this paper discusses the basic features of geological structure in Hulun Buir area,Inner Mongolia.