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Leye-Fengshan, A New Applicant of Global Geopark in Guangxi, China

机译:中国广西全球地质公园的新申请人乐业-凤山

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摘要

Leye-Fengshan Geopark in Leye County and Fengshan County in the northwestern Guangxi,China,is in the transitional slope zone from southeastern Yunnan-Cuizhou Plateau to Guangxi Basin. It has an area of nearly 900 km2 in the subtropic monsoon climatic region and in neo-tectonic uplifting area. The geopark exposes Devonian to Neogene carbonate and clastic rocks, including a continuous sequence of Devonian to Permian carbonate rocks more than 3000 m thick. Clastic rocks surround the exposed karst and lots of allogenic water from clastic areas flow into karst areas with S type geological structure and rhombus geological structure,and they developed two big subterranean river systems in karst inlier areas, i. e. Bailang subterranean river system and Poxin subterranean river system with 81.5 km and 162 km long, they controlled the development of karst tiankeng group and very large caves (cave chambers)respectively.There are mainly 4 kinds of geologic formations in Leye-Fengshan Geopark, tiankeng ( great do-lines) ,caves(large cave chambers) ,karst gorge,Fengcong( high cone karst)and poljes. Tiankeng is the great doline with vertical cliffs around, with more than 100m in entrance diameter and in depth;it is mostly related with subterranean river at the bottom of doline. There are 27 tiankengs developed in Bailang subterranean river drainage area, which is the biggest tiankeng group in the world. Of them Dashiwei is the biggest, it is 600×420m in diameter and 613m deep at most,70000000 m3 in volume and 100000 m2 of sub-primeval forest in area. There are more than 100 caves in the geopark, Jiangzhou cave is the biggest,with 42.5km in length, 11400000 m2 in cave floor area and 28.9M m3 in volume. It formed 24 cave chambers with more than 10000 m2 in floor area, Hongmeigui cave chamber is the largest, with 50000 m2 in area,Sunlight cave chamber is the highest,with 365m high at most and 260m high in average. It is the most concentrated cave chambers area in the world for 7 of 23 cave chambers with more than 25000 m2 is here. There are also lots of light through caves and natural bridges;in particular Buliu natural bridge and Jiangzhou natural bridge are the biggest and the second biggest one in span in the world,with 177m and 144m respectively. It features typical Fengcong(cone karst)in the geopark,with about 1000m asl and 150~500m height difference between peaks and depressions,as well as lots of poljes developed between karst area and nonkarst area, for allogenic water from clastic area is more aggressive.
机译:广西西北部的乐业县和凤山县的乐业-凤山地质公园位于云南-黔州高原东南部至广西盆地的过渡斜坡带。它在亚热带季风气候区和新构造隆升区的面积近900平方公里。该地质公园使泥盆纪暴露于新近纪的碳酸盐岩和碎屑岩,其中包括厚度超过3000 m的泥盆纪至二叠纪碳酸盐岩的连续序列。碎屑岩围绕裸露的岩溶,碎屑区的大量异水流入具有S型地质结构和菱形地质结构的岩溶区,并在岩溶内陆区发展了两条大的地下河系。 e。分别有81.5 km和162 km长的白浪地下河系统和Poxin地下河系统分别控制着喀斯特天坑群的发育和非常大的溶洞(洞穴室)的发展。天坑里耶—凤山地质公园主要有4种地质构造。 (大岩溶线),洞穴(大洞穴洞室),喀斯特峡谷,峰丛(高锥岩溶)和波尔杰斯。天坑是一条巨大的龙猫,周围有垂直的悬崖,入口直径和深度都超过100m;它主要与龙猫底部的地下河有关。白浪地下河流域开发了27个天坑,是世界上最大的天坑群。其中大石围最大,直径为600×420m,最大深度为613m,体积为7000万立方米,面积为10万平方米。地质公园内有100多个溶洞,其中最大的是江州溶洞,全长42.5公里,溶洞面积1140万平方米,容积2890万立方米。它形成了24个洞室,占地面积10000平方米以上,其中红梅桂洞室最大,面积为50000平方米,阳光洞室最大,最高365m,平均高度260m。这是世界上最集中的洞室区域,这里是23个洞室中的7个,面积超过25000平方米。穿过山洞和天然桥的光线也很多,特别是不流天然桥和江州天然桥是世界上跨度最大和第二大的桥,分别为177m和144m。它具有典型的地质公园峰丛(岩溶),山峰与洼地之间的高度差约为1000m,且峰高与凹陷之间的高度差为150〜500m,并且岩溶区与非岩溶区之间发育有许多poljes,因为碎屑区的异源水更具侵蚀性。

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