摘要
秦岭终南山地质公园地处西安市南,总面积1074.85 km2。素有"中国人的中央公园"之称的秦岭造山带,是全球典型的复合型大陆造山带之一,是形成统一中国大陆的主要结合带,是中国南北天然的地质、地理、生态、气候、环境乃至人文的分界线。秦岭终南山地质公园地处秦岭造山带的主体部位,是中央造山带的经典地段。依次分布有:翠华山山崩地貌与佛教文化园区、骊山裂谷地垒构造园区、冰晶顶韧性剪切带与构造混合岩化园区、玉山岛弧型花岗岩峰岭地貌园区、南太白板块碰撞缝合带与第四纪冰川园区等五个各具特色主题又互相联系的园区和黑河、沣峪两条科学考察路线。是至今为止距大都市最近的地质公园。
The Qinling Zhongnanshan Geopark is situated in the south of Xi＇ an city, covering an area of 1074.85 square kilometers. The Qinling Orogenic belt is reputed as ＂ the central park of Chinese people＂, which is one of typical complex continental orogenic belts in the world and a major juncture zone combining the territory of China together. It is also a natural boundary forming different geology, geography, weather, environment and culture in north and south of China. The Qinling Zhongnanshan Geopark lies in the central part of the Qinling Orogenic belt, showing the most representative portion of the central orogenic belt in China. The geopark is divided into five sub-geoparks with distinct local characteristics and two geotoure lines. They are Cuihuashan Mountain collapse-slide landscape, Lishan rift-graben structures, Bingjingding ductile shearing zone and tectonic migmatite, Yushan island-arc granitic peaks and ridges, South Taibai plate collision suture zone and Quaternary glacier park, and Heihe and Fengyu geotour lines. So far in the world, the geopark is the nearest one to a metropolis.
出处
《陕西地质》
2009年第2期103-108,共6页
Geology of Shaanxi
关键词
秦岭
终南山
地质公园
造山带
地质遗迹
旅游资源开发
Qinling
Zhongnanshan
geopark
orogenic zone
geoheritage
development of tourist resources
