江西三清山花岗岩峰林地质公园特征及评价

Characteristic evaluation of granite peaks geological park in Sanqingshan Mountain,Jiangxi Province

三清山位处扬子板块与华夏板块结合带,区内花岗岩受北东、北西和北东东向三条断裂控制,形成典型的三角形断块山,地貌处于幼年晚期至壮年早期发育阶段。园区内花岗岩峰峦、峰丛、峰墙、峰柱、石芽及造型石等微地貌景观发育,类型齐全,分布集中,集结了花岗岩峰林地貌的精华,为世界罕见;兼具千年道教文化和秀美自然风光,具有极高的科研、科普和旅游观赏价值。

Sanqingshan Mountain is situated in the contact belt between the Yangtze Plate and the Cathaysian Plate. Granites are dominated by three fractures （northeastward and northwestward and northeast- eastward fractures） in the region,forming typical triangle mountain of break block. The geomorphologic landscape is corresponding to development stage between later childhood period and early mature stage. Geomorphologic landscape is well-developed and various styles of ridges, peak cluster, peak wall, peak column and karen as well as modeling rock of granite in the park, which is unique in the world. The park possesses great value of scientific research, scientific popularization and tourism for its Taoism civilization for a thousand years and elegant natural scenes.