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.