干旱区生态环境知识资源中心(Arid): 则岔石林地质公园喀斯特地貌类型及形成机制

Arid

	则岔石林地质公园喀斯特地貌类型及形成机制
其他题名	Geomorphic types and formation mechanism of the Karst landform in Zecha Stone Forest Geopark
	徐家红 1; 鄢志武 2; 柳晓丹 3
来源期刊	干旱区地理
ISSN	1000-6060
出版年	2018
卷号	41 期号:5 页码:1027-1034
中文摘要	则岔石林地质公园位于甘肃省碌曲县,该处地貌完整地保存了高寒喀斯特的特征,具有典型性与稀有性。为了揭示其自然科学价值,促进自然资源开发与景观保护,基于前人工作基础,通过野外地质调查,以碌曲县区域地学为背景,介绍了则岔石林地质公园的喀斯特地貌类型,即以高原石林为主,一线天为亮点,小型溶洞为辅。继而从地质构造、岩性、水文气候、生物因素四方面分析了园内喀斯特地貌的形成机制。对完善我国高海拔地区岩溶系列地质遗迹的科学研究具有一定意义。同时,高寒喀斯特的生态化对南方喀斯特沙漠化的治理具有良好的示范作用。
英文摘要	Zecha Stone Forest Geopark is located in Luqu County,Gansu Province,China.The landform in this area keeps the intact features of alpine-arctic karst,with typicality and rarity.In order to reveal its natural and scientific value,and to promote the natural resource development and landscape protection,the regional geological and geographic backgrounds of Luqu are briefed based on previous work and field investigation.The types of karst landform in Zecha Stone Forest Geopark have been introduced,which include the highland stone forest as the majority,the thin strip of sky as lightspot and the small karst caves as complementarities.The formation mechanism of the karst landform has been further analyzed from four aspects:tectonics,lithology,climate and biology.The results show that the tectonic movement,the development of joint fissures,and the difference of rocks cementation degrees laid a foundation for the formation of karst landscape.Moreover,under the alpine-arctic and dank climate condition with great changes,water corrosion,frost denudation,and weathering formed the unique alpine-arctic karst landscape in this area,which was characterized by many bedrocks and steep walls,tall stone forest and pillars,a few karst caves with poor connectivity and small size.The research provided some academic information of the karst landform in Zecha Stone Forest Geopark,which has certain significance in the scientific research on karst geological relics in high altitude areas of China.The ecologicalization of alpine-arctic karst provided a good reference for the governance of karst desertification in the south part of China.
中文关键词	喀斯特地貌 ; 形成机制 ; 石林 ; 青藏高原东部 ; 碌曲
英文关键词	Karst landform formation mechanism stone forest Eastern Qinghai-Tibet Plateau Luqu
语种	中文
国家	中国
收录类别	CSCD
WOS类目	GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向	Geology
CSCD记录号	CSCD:6345194
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/237607
作者单位	1.忻州师范学院旅游管理系, 忻州, 山西 034000, 中国; 2.中国地质大学(武汉)经济管理学院, 武汉, 湖北 430000, 中国; 3.武警黄金第七支队, 烟台, 山东 264000, 中国
推荐引用方式 GB/T 7714	徐家红,鄢志武,柳晓丹. 则岔石林地质公园喀斯特地貌类型及形成机制[J],2018,41(5):1027-1034.
APA	徐家红,鄢志武,&柳晓丹.(2018).则岔石林地质公园喀斯特地貌类型及形成机制.干旱区地理,41(5),1027-1034.
MLA	徐家红,et al."则岔石林地质公园喀斯特地貌类型及形成机制".干旱区地理 41.5(2018):1027-1034.