则岔石林地质公园喀斯特地貌类型及形成机制

doi:10.12118/j.issn.1000-6060.2018.05.15

干旱区地理 ›› 2018, Vol. 41 ›› Issue (5): 1027-1034.doi: 10.12118/j.issn.1000-6060.2018.05.15

则岔石林地质公园喀斯特地貌类型及形成机制

徐家红¹, 鄢志武², 柳晓丹³

1 忻州师范学院旅游管理系, 山西忻州 034000;
2 中国地质大学(武汉)经济管理学院, 湖北武汉 430000;
3 武警黄金第七支队, 山东烟台 264000

收稿日期:2018-04-15 修回日期:2018-07-15 出版日期:2018-09-25
通讯作者: 鄢志武(1963-),男,硕士,教授,主要从事旅游地学、地质公园方面的研究和教学.E-mail:jhxu0821@cug.edu.cn
作者简介:徐家红(1986-),女,硕士,助教,主要从事旅游地理方面的研究和教学.E-mail:jhxu0821@163.com
基金资助:
甘肃碌曲国家地质公园调研及规划设计（108-KH116312）

Geomorphic types and formation mechanism of the Karst landform in Zecha Stone Forest Geopark

XU Jia-hong¹, YAN Zhi-wu², LIU Xiao-dan³

1 Department of Tourism Management, Xinzhou Normal University, Xinzhou 034000, Shanxi, China;
2 School of Economics and Management, China University of Geosciences, Wuhan 430000, Hubei, China;
3 Chinese People's Armed Police Gold Force Team 7, Yantai 264000, Shandong, China

Received:2018-04-15 Revised:2018-07-15 Online:2018-09-25

摘要/Abstract

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。

关键词: 喀斯特地貌, 形成机制, 石林, 青藏高原东部, 碌曲

Abstract: 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.

Key words: Karst landform, formation mechanism, stone forest, Eastern Qinghai-Tibet Plateau, Luqu

中图分类号:

P931.5

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]. 干旱区地理, 2018, 41(5): 1027-1034.

XU Jia-hong, YAN Zhi-wu, LIU Xiao-dan. Geomorphic types and formation mechanism of the Karst landform in Zecha Stone Forest Geopark[J]. 干旱区地理, 2018, 41(5): 1027-1034.

参考文献

[1] 梁旺俊,罗爱昌.碌曲县志[M].兰州:甘肃文化出版社,2006:79-83.[LIANG Wangjun,LUO Aichang.Annals of Luqu County[M].Lanzhou:Gansu Culture Press,2006:79-83.]
[2] 鄢志武,韩道山,罗伟,等.甘肃碌曲则岔石林地质公园综合考察报告[R]. 武汉:中国地质大学,2013:35.[YAN Zhiwu,HAN Daoshan,LUO Wei,et al.Comprehensive report on Zecha Shilin Geopark in Luqu County Gansu Province[R].Wuhan:China University of Geosciences,2013:35.]
[3] 陈安泽,钱方,李兴中,等.中国喀斯特石林景观研究[M].北京:科学出版社,2011:19-20.[CHEN Anze,QIAN Fang,LI Xingzhong,et al.Karst stone forest landscapes in China[M].Beijing:Science Press,2011:19-20.]
[4] 高全洲,崔之久,刘耕年,等.晚新生代青藏高原岩溶地貌及其演化[J].古地理学报,2001,3(1):85-90+102.[GAO Quanzhou,CUI Zhijiu,LIU Gengnian,et al.Late Cenozoic Karst landforms on Qinghai-Tibet Plateau and their evolution[J].Journal of Palaeogeography,2001,3(1):85-90+102.]
[5] 陈安泽,钱方,李兴中,等.中国喀斯特石林景观研究[M].北京:科学出版社,2011:27.[CHEN Anze,QIAN Fang,LI Xingzhong,et al.Karst stone forest landscapes in China[M].Beijing:Science Press,2011:27.]
[6] 王数,东野光亮.地质学与地貌学[M].2版.北京:中国农业大学出版社,2013:97-99.[WANG Shu,DONGYE Guangliang.Geology and geomorphology[M].2^nd ed.Beijing:China Agricultural University Press,2013:97-99.]
[7] 左俊辉,罗群,郭喜梅.中国地貌三大阶梯对喀斯特发育的若干影响——以中国西南岩溶区为例[J].科技信息,2012,(18):210-211+213.[ZUO Junhui,LUO Qun,GUO Ximei.How the three gradient terrains of Chinese landform affect the development of Karst landform:Taking the Karst areas in southwest China as an example[J].Science & Technology Information,2012,(18):210-211+213.]
[8] 崔之久,高全洲,刘耕年,等.青藏高原夷平面与岩溶时代及其起始高度[J].科学通报,1996,41(15):1402-1406.[CUI Zhijiu,GAO Quanzhou,LIU Gengnian,et al.Planation surface,Karst era and its height of Qinghai-Tibet Plateau[J].Chinese Science Bulletin,1996,41(15):1402-1406.]
[9] 贾承造,何登发,陆洁民.中国喜马拉雅运动的期次及其动力学背景[J].石油与天然气地质,2004,25(2):121-125+169.[JIA Chengzao,HE Dengfa,LU Jiemin.Periods and dynamic background of China's Himalayan movement[J].Oil & Gas Geology,2004,25(2):121-125+169.]
[10] 卢耀如,杰显义,张上林,等.中国岩溶(喀斯特)发育规律及其若干水文地质工程地质条件[J].地质学报,1973,(1):121-136+141.[LU Yaoru,JIE Xianyi,ZHANG Shanglin,et al.Development laws and its hydrogeological engineering geological conditions of China Karst[J].Acta Geologica Sinica,1973,(1):121-136+141.]
[11] 鄢志武,韩道山,罗伟,等.甘肃碌曲则岔石林地质公园综合考察报告[R].武汉:中国地质大学,2013:36-39.[YAN Zhiwu,HAN Daoshan,LUO Wei,et al.Comprehensive report on Zecha Shilin Geopark in Luqu County Gansu Province[R].Wuhan:China University of Geosciences,2013:36-39.]
[12] 伍光和.自然地理学[M].4版.北京:高等教育出版社,2008:275.[WU Guanghe.Physical geography[M].4^th ed.Beijing:Higher Education Press,2008:275.]
[13] 景春刚.洮河-碌曲水文站水文特性分析[J].甘肃科技,2010,26(22):78-79.[JING Chungang.Analysis of hydrologic characteristics in Tao River-Luqu hydrologic station[J].Gansu Science and Technology,2010,26(22):78-79.]
[14] 樊维,陈洪凯.裂隙岩体植物根劈机理研究[J].科技创新导报,2015,(35):46-47.[FAN Wei,CHEN Hongkai.Research on root wedging mechanism of plant in jointed rocks[J].Science and Technology Innovation Herald,2015,(35):46-47.]
[15] 卢耀如.中国南方喀斯特发育基本规律的初步研究[J].地质学报,1965,45(1):108-129.[LU Yaoru.Preliminary investigation of some main features of Karst development in south China[J].Acta Geologica Sinica,1965,45(1):108-129.]
[16] 袁道先.中国岩溶学[M].北京:地质出版社,1993:29-33.[YUAN Daoxian.Chinese Karst[M].Beijing:Geological Publishing House,1993:29-33.]
[17] 陈安泽,余国元,王祥义.喀斯特旅游资源基础理论与开发研究[M].北京:地震出版社,2004:67-82.[CHEN Anze,YU Guoyuan,WANG Xiangyi.Basic theory and development research on Karst tourism resources[M].Beijing:Seismological Press,2004:67-82.]
[18] 李玉辉.中国云南石林岩溶形态特征与类型[J].中国岩溶,2002,21(3):165-172.[LI Yuhui.Morphological tipes and their features of Shilin Karst in Yunnan,China[J].Carsologica Sinica,2002,21(3):165-172.]
[19] CAO Jianhua,YUAN Daoxian,TONG Liqiang,et al.An overview of Karst ecosystem in southwest China:Current state and future management[J].Journal of Resources and Ecology,2015,6(4):247-256.
[20] 崔之久,洪云,高全洲,等.青藏高原东北部古喀斯特过程与环境[J].地理学报,1996,51(5):408-417.[CUI Zhijiu,HONG Yun,GAO Quanzhou,et al.The process and environment of polaeokarst in the northeast area of Qinghai-Xizang Plateau[J].Acta Geographica Sinica,1996,51(5):408-417.]
[21] 李德文,崔之久,刘耕年.青藏高原古岩溶的存在及其与东邻地区岩溶的对比[J].中国岩溶,1999,18(4):25-34.[LI Dewen,CUI Zhijiu,LIU Gengnian.Existence of palaeokarst on Tibet Plateau and its correlation with the Karst of the eastern district[J].Carsologica Sinica,1999,18(4):25-34.]
[22] 高全洲,崔之久,陶贞,等.青藏高原古岩溶的性质、发育时代和环境特征[J].地理学报,2002,57(3):267-274.[GAO Quanzhou,CUI Zhijiu,TAO Zhen,et al.The nature,formation age and genetic environment of the palaeokarst on the Qinghai-Xizang Plateau[J].Acta Geographica Sinica,2002,57(3):267-274.]