拉萨扎叶巴沟自然资源与旅游开发研究  

Natural Resources and Tourism Development of Zhayeba Gully in Lhasa

作　　者：于涛[1] 古格·其美多吉[1] 张薇薇 YU Tao;GUGE Qimeiduoji;ZHANG Weiwei(College of Science,Tibet University)

机构地区：[1]西藏大学理学院,西藏拉萨市850000

出　　处：《现代矿业》2022年第5期6-9,共4页Modern Mining

摘　　要：我国的岩溶区面积广大、分布广泛,岩溶地貌类型多种多样。拉萨市区周边的喀斯特属于高原高山岩溶。通过前人考察和研究,发现在拉萨周围零星存在古喀斯特地貌。对其进行深入研究,能为拉萨市的国土整治与规划、自然地理区划、旅游资源开发、箱体地理教学等提供基础资料和科学依据。扎叶巴沟内的喀斯特地貌的典型性与规模虽不及云贵高原,但是具有高原特色,尤其是许多溶洞已开辟为修行洞及小庙,开辟历史悠久,文化底蕴深厚,成为拉萨旅游的一颗明珠。为促进西藏地区旅游地质发展,对拉萨市东北部的扎叶巴沟内的自然地理和村落分布特点以及曲普沟内石灰岩峰丛和溶沟等进行了调查与分析,认为其成因与拉萨周边的喀斯特地貌成因相似。China’s karst areas are vast and widely distributed,and the types of karst landforms are diverse.The karst around the city of Lhasa belongs to the plateau alpine karst.Through the investigation and study of many geologists,it was found that there were sporadic ancient karst landforms around Lhasa.Indepth study can provide basic information and scientific basis for the land consolidation and planning,physical geography zoning,tourism resource development,and box geography teaching in Lhasa.Although the typical and scale of the karst landform in Zhayeba gully is not as good as that of the Yunnan-Guizhou Plateau,it has the characteristics of the plateau,especially many caves have been opened into practice caves and small temples,with a long history and profound cultural heritage,and have become a pearl of Lhasa tourism.In order to promote the development of tourism geology in Tibet,this paper investigates the natural geography and village distribution characteristics of Zhayeba gully in the northeast of Lhasa City,as well as the limestone peaks and dissolving ditches in the Qupu Ditch,the causes of which are similar to the karst geomorphological causes around Lhasa.

关 键 词：扎叶巴沟 古喀斯特地貌 旅游开发 

分 类 号：F592.7[经济管理—旅游管理]