[1]陈留勤,占义勇,潘志新,等.江西赣州石城国家地质公园丹霞地貌特征及旅游开发[J].华东地质,2020,41(04):387-395.[doi:10.16788/j.hddz.32-1865/P.2020.04.010]
　CHEN Liu-qin,ZHAN Yi-yong,et al.Danxia landforms and tourism development in Shicheng National Geopark, Jiangxi Province[J].East China Geology,2020,41(04):387-395.[doi:10.16788/j.hddz.32-1865/P.2020.04.010]
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江西赣州石城国家地质公园丹霞地貌特征及旅游开发()
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《华东地质》[ISSN:2096-1871/CN:32-1865/P]

卷:
41
期数:
2020年04期
页码:
387-395
栏目:
地质公园及地质遗迹
出版日期:
2020-12-20

文章信息/Info

Title:
Danxia landforms and tourism development in Shicheng National Geopark, Jiangxi Province
文章编号:
2096-1871(2020)04-387-09
作者:
陈留勤 2; 占义勇2; 潘志新3; 张鹏琼2
（1. 东华理工大学 核资源与环境国家重点实验室，南昌 330013；2. 东华理工大学 地球科学学院，南昌 330013；3. 海南大学 旅游学院，海口 570228）
Author(s):
CHEN Liu-qin1;  2;  ZHAN Yi-yong2;  PAN Zhi-xin3;  ZHANG Peng-qiong2
(1. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China; 2. School of Earth Sciences, East China University of Technology, Nanchang 330013, China; 3. School of Tourism, Hainan University, Haikou 570228, China)
关键词:
关键词: 丹霞地貌;  龟裂地貌;  地质遗迹;  石城国家地质公园;  旅游开发
Keywords:
Key words:Danxia landscape;  polygonal cracks;  geoheritage;  Shicheng National Geopark;  tourism development
分类号:
P901 P931.2
DOI:
10.16788/j.hddz.32-1865/P.2020.04.010
文献标志码:
A
摘要:
摘要: 石城国家地质公园位于江西省赣州市,以丹霞地貌景观为主要旅游资源,以发育在红色砂岩中的龟裂地貌为特色。不同类型的龟裂地貌组合成为栩栩如生的象形景观,尤以龟寿石和仙人犁田最引人注目。通过野外地质调查,总结了园区丹霞地貌景观类型和特征,认为它们主要是晚白垩世陆相红层受到构造抬升、断裂切割、岩性组成、流水侵蚀及风化作用形成的,砂岩独特的龟裂地貌主要是风化作用的结果。近些年来,石城国家地质公园旅游发展虽然取得了明显进步,但主要还停留在观光旅游层面。在国家提倡科普教育、研学旅行的背景下,园区应与广东丹霞山、福建泰宁、江西龙虎山等世界地质公园开展交流与合作,借鉴成功经验; 增加科研投入,为提升景区研学质量提供基础研究资料。
Abstract:
Abstract:The Shicheng National Geopark is located in Ganzhou City of Jiangxi Province, with Danxia landscapes as the main tourism resources and distinguished by polygonal cracks on red sandstone outcrops. A variety of iconic landforms are formed by spatial arrangement of polygonal cracks, among which the Guishou(giant turtle-like)stone and Xianrenlitian(large regular cracking)scenery sites are the most fascinating. The types and features of Danxia landscapes are summarized through field geological survey in the geopark. The results show that the Danxia landscapes are mainly formed by the combination of tectonic uplift, fault incision, lithology, fluvial erosion and weathering of the terrestrial Late Cretaceous red beds. The peculiar polygonal cracks are mainly produced by weathering. In recent years, the geopark has made significant progress in tourism development, but remains at the level of sightseeing tour. Under the background of national call for science popularization education and learning trips, it is necessary for the geopark to conduct close communication and cooperation with the Danxiashan of Guangdong, Taining of Fujian, and Longhushan of Jiangxi Provinces to learn successful experiences. Meanwhile, it is suggested the investment on scientific research should be increased to provide basic research data for improving the quality of learning trips.

参考文献/References:

[1] 陈国达,刘辉泗.江西贡水流域地质[J].江西地质汇刊,1939(2):164.
[2] PENG H. China Danxia [M]. Beijing: Higher Education Press, 2020: 1-391.
[3] 郭福生,陈留勤,严兆彬,等.丹霞地貌定义、分类及丹霞作用研究[J].地质学报,2020,94(2):361-374.
[4] 朱诚,马春梅,张广胜,等.中国典型丹霞地貌成因研究[M].北京:科学出版社,2015:1-348.
[5] 潘志新,任舫,彭华. 美国西部红层地貌发育及与中国东南部丹霞地貌的对比[J]. 地理研究,2018,37(12): 2399-2410.
[6] 章桂芳,陈凯伦,张浩然,等.基于DEM的丹霞地貌演化阶段划分[J].中山大学学报(自然科学版),2018,57(2):12-21.
[7] 许应石,郭刚,孙欣欣. 南京栖霞山地质遗迹调查与地质公园建设[J]. 华东地质,2018,39(1):73-80.
[8] 陈同刚,朱将波,汪启年,等. 江西宁都丹霞地貌地质特征及成因分析[J]. 华东地质,2019,40(1):27-34.
[9] CHEN L Q, GUO F S, LIU F J, et al. Origin of Tafoni in the Late Cretaceous aeolian sandstones, Danxiashan UNESCO Global Geopark, South China [J]. Acta Geologica Sinica, 2019, 93(2): 451-463.
[10] YAN L B, PENG H, ZHANG S Y, et al. The spatial patterns of Red Beds and Danxia Landforms: Implication for the formation factors-China [J]. Scientific Reports, 2019, 9(1): 1961.
[11] 曹珂.中国陆相白垩系地层对比[J]. 地质论评,2013,59(1): 24-40.
[12] 黄进.石城丹霞地貌[M]. 北京:科学出版社,2012:1-180.
[13] 黄进.丹霞地貌坡面发育的一种基本方式[J].热带地貌,1982,3(2):107-134.
[14] YOUNG R W, WRAY R A L, YOUNG A R M. Sandstone Landforms [M]. Cambridge: Cambridge University Press, 2009.
[15] NEAL J T, LANGEE A M, KERR P F. Giant desiccation polygons of Great Basin Playas[J]. Geological Society of America Bulletin, 1968, 79: 69-90.
[16] EI MAARRY M R, KODIKARA J, WIJESSORIYA S, et al. Desiccation mechanism for formation of giant polygons on Earth and intermediate-sized polygons on Mars: Results from a pre-fracture model [J]. Earth and Planetary Science Letters, 2012, 323/324: 19-26.
[17] PARADISE T R. Tafoni and other rock basins[C]//SHRODER J, POPE G A. Treatise on Geomorphology. San Diego, CA: Academic Press, 2013: 111-126.
[18] 吕洪波,苏德辰,章雨旭,等. 中国不同气候带盐风化作用的地貌特征[J]. 地质论评,2017,63(4):911-926.
[19] MIGON P, GOUDIE A. Sandstone Geomorphology of South-West Jordan, Middle East [J]. Quaestiones Geographicae, 2014, 33(2): 119-126.
[20] YOUNG R W, WRAY R A L. Rock control in sandstone geomorphology: a tribute to Eiju Yatsu with some Australian examples [J]. Zeitschrift Geomorphologie, 2015, 59(1): 3-17.
[21] CHEN L Q, GUO F S, STEEL R J, et al. Petrography and geochemistry of the Late Cretaceous redbeds in the Gan-Hang Belt, southeast China: implications for provenance, source weathering, and tectonic setting [J]. International Geology Review, 2016, 58(10): 1196-1214.
[22] CHEN L Q, STEEL R J, GUO F S, et al. Alluvial fan facies of the Yongchong Basin: Implications for tectonic and paleoclimatic changes during Late Cretaceous in SE China [J]. Journal of Asian Earth Sciences, 2017, 134: 37-54.
[23] GUO F S, CHEN L Q, XU H, et al. Origin of beaded tafoni in cliffs of Danxia landscapes, Longhushan Global Geopark, South China [J]. Journal of Mountain Science, 2018, 15(11): 2398-2408.
[24] 郭福生,姜勇彪,胡中华,等.龙虎山世界地质公园丹霞地貌成景系统特征及其演化[J].山地学报,2011,29(2):195-201.
[25] 姜勇彪,郭福生,陈珊珊.江西信江盆地丹霞地貌空间分布及其成因[J].山地学报,2013,31(6):731-737.
[26] 李霞,何庆成,董颖,等.贵州赤水南部地区丹霞地貌类型特征及成因演化分析[J].地球学报,2013,34(4):501-508.
[27] 陈留勤,刘富军,郭福生,等.丹霞山地学实习教程[M].北京:地质出版社,2019:1-143.
[28] DORN R I, DORN J, HARRISON E, et al. Case hardening vignettes from the western USA: convergence of form as a result of divergent hardening processes [J]. Yearbook of the Association of Pacific Coast Geographers, 2012, 74(1): 53-75.
[29] DORN R I, MAHANEY W C, KRINSLEY D H. Case Hardening: Turning Weathering Rinds into Protective Shells [J]. Elements, 2017, 13(3): 165-169.
[30] 张鹏琼,陈留勤,郭福生,等.江西石城国家地质公园龟裂地貌特征及成因分析[J].地球学报,2020,41(1):117-126.
[31] PARADISE T R. Disparate sandstone weathering beneath lichens, Red Mountain, Arizona [J]. Geografiska Annaler, 1997, 79(3): 177-184.
[32] THOMAS R. Analysis of sandstone weathering of the ‘Roman’ Theater in Petra, Jordan [J]. Journal of Molecular Spectroscopy, 1999, 205(43): 319-322.

备注/Memo

备注/Memo:
*收稿日期:2020-02-01 修订日期:2020-04-10 责任编辑:谭桂丽
基金项目:国家自然科学基金“赣粤闽地区丹霞地貌形成与演化过程中岩相控制作用研究(编号:41772197)”、“中国西北部干旱区和东南部湿润区丹霞地貌发育机制的对比研究(编号:41761002)”项目联合资助。
第一作者简介:陈留勤,1983年生,男,副教授,主要从事红层与丹霞地貌研究。Email:275218175@qq.com。
通信作者简介:潘志新,1986年生,男,讲师,主要从事丹霞地貌、地质遗迹保护与开发研究。Email:415979045@qq.com。
更新日期/Last Update: 2020-11-19