首页> 外文会议>The First International Conference on Geoparks(第一届世界地质公园大会) >Geological Historical Remains and Geological Background In Yuntaishan World Geopark
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Geological Historical Remains and Geological Background In Yuntaishan World Geopark

机译:云台山世界地质公园的地质历史遗迹和地质背景

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1 IntroductionIn March 2004, the world geopark meeting hold in French Paris consistently passes through Yuntaishan national geopark on meeting to become one of first world geoparks. This world geopark is consisted of 5 landscapes (localities), which are located in the north part of Jiaozuo, Henan Province. The Yuntaishan World Geopark is a comprehensive geopark mainly with tectonic structures and the geological historical remains that was formed by Eastern Asia Rift. The Geographic coordinate is E113°22'707"- 114°14'079", N35°21'323"-35°24'966", the area is approximately 500km2, which is also located at the most south end of the Taihangshan Range, and it is growth in the turn place of the second steps of Chinese landforms and the alluvial plain of North China (Fig. 1).
机译:1引言2004年3月,在法国巴黎举行的世界地质公园会议不断通过云台山国家地质公园,成为世界上最早的世界地质公园之一。这个世界地质公园由5个景观(地区)组成,位于河南省焦作市的北部。云台山世界地质公园是一个综合性的地质公园,主要具有构造构造和东亚大裂谷形成的地质历史遗迹。地理坐标为E113°22'707“-114°14'079”,N35°21'323“ -35°24'966”,面积约为500平方公里,也位于太行山的最南端范围,它是中国地貌第二阶段和华北冲积平原转折处的增长(图1)。

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