[1]谭艳,朱诚,吴立,等.广东丹霞山砂岩蜂窝状洞穴及白斑成因[J].山地学报,2015,(03):279.
 TAN Yan,ZHU Cheng,WU Li,et al.Geomophogensis on Sandstone Honeycombs and White Spot in the Mt. Danxiashan,Guangdong Province,South China[J].Mountain Research,2015,(03):279.
点击复制

广东丹霞山砂岩蜂窝状洞穴及白斑成因()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年03期
页码:
279
栏目:
山地研究
出版日期:
2015-06-01

文章信息/Info

Title:
Geomophogensis on Sandstone Honeycombs and White Spot in the Mt. Danxiashan,Guangdong Province,South China
作者:
谭艳;朱诚;吴立;孙伟;王晓翠;贾天骄;彭华;侯荣丰;
南京大学地理与海洋科学学院;安徽师范大学国土资源与旅游学院;中国科学院南京地理与湖泊研究所;中山大学地理科学与规划学院;丹霞山风景名胜区管理委员会;
Author(s):
TAN YanZHU ChengWU LiSUN WeiWANG Xiaocui JIA TianjiaoPENG HuaHOU Rongfeng
1. School of Geographic and Oceanographic Science,Nanjing University,Nanjing 210093,Jiangsu,China; 2. College of Territorial Resources and Tourism,Anhui Normal University,Wuhu 241002,Anhui,China; 3. Nanjing Institute of Geography & Limnology,Chinese Academy of Sciences,Nanjing 210008,Jiangsu,China; 4. School of Geography and Planning,Sun Yat-sen University,510275,Guangzhou,China 5. Administrative Committee of Danxiashan Scenic Spot,Shaoguan 512300,Guangdong,China
关键词:
广东丹霞山砂岩成分分析蜂窝状洞穴白斑
Keywords:
Mt. Danxiashansandstonecomponent analysishoneycombswhite spot
分类号:
P931
文献标志码:
A
摘要:
为研究广东韶关市丹霞山砂岩蜂窝状洞穴及白斑成因,对世界自然遗产地丹霞山景区内玉女拦江洞中采集的6个砂岩蜂窝状洞穴样品,以及在鸭麻岩地区采集的4个白斑样品,进行XRF和ICP-MS元素地球化学分析及岩石薄片偏光显微镜鉴定。结果表明,发育蜂窝状洞穴的砂岩体与其基岩砂岩体的成分含量相近,岩体内部成分差异不是蜂窝状洞穴的成因。综合分析认为,丹霞山砂岩蜂窝状洞穴的产生是岩石的矿物组成及结构、洞穴所在的地形条件、气候因素和蜂窝状洞穴所形成的微气候共同作用的结果。对白斑的元素分析结果显示,发育白斑的砂岩在成岩过程中,红色基岩形成于氧化环境,而白斑形成于还原环境中,赤铁矿被还原形成白斑。
Abstract:
Abundant typical sandstone morphologic shapes developed in Mt. Danxiashan. We collected six samples of sandstone honeycombs in Yunülanjiang Cave and four samples of white spots in Yamayan to do component analysis (XRF and ICP-MS) with the purpose of explaining their genesis. The results indicate that the component contents of samples in honeycombs and bedrock are similar so that there is no direct relationship between lithological differences and honeycomb’s formation. The comprehensive analysis reveals that honeycombs are the result of physical weathering. And the rock structure,topography,climate and cavern microclimate are important influencing factors in the formation process of honeycombs. In the discussion of sandstone white spot,reducing conditions prevail in the process and some minerals are dissolved. Reduction of Fe making the color change from red to white with water percolating through the rock,thereby forming a white spot on the surface.

参考文献/References:

[1] Yang Zaitian. On Xu Xiake’s investigation into China’s Danxia Landform——Memory Xu Xiake 360 anniversary [J]. Geographical Research,2000,19(4):429-436 [杨载田. 徐霞客对我国丹霞地貌旅行考察的贡献——纪念徐霞客逝世360周年[J] . 地理研究,2000,19(4):429-436]
[2] Feng Jinglan,Zhu Huisheng,Zheng Jingyun. Geological minerals of Nanxiong,Shixing,Renhua,Qujiang in Guangdong [J]. Geological Annual Report of Institute of Geologic Survey of Guangdong & Guangxi,1928,(1):38-42 [冯景兰,朱翙声. 广东曲江仁化始兴南雄地质矿产[J]. 两广地质调查所地质年报,1928,(1):38-42]
[3] Chen Guoda. Red rock systems of Guangdong Province [J]. The Science Quarterly of the National Sun Yat-Sen University,1935,6(4):1-30 [陈国达. 广东之红色岩系[J]. 国立中山大学理学季刊,1935,6(4):1-30]
[4] Zeng Zhaoxuan,Huang Shaomin. Red bed in southeastern China [J]. Journal of South China Normal University:Natural Science,1978,(1):56-73 [曾昭璇,黄少敏. 中国东南部红层地貌[J]. 华南师范学院学报:自然科学,1978,(1):56-73]
[5] Zeng Zhaoxuan,Huang Shaomin. Red bed in southeastern China (Sequel) [J]. Journal of South China Normal University:Natural Science,1978,(2):40-54 [曾昭璇,黄少敏. 中国东南部红层地貌(续)[J]. 华南师范学院学报:自然科学版,1978,(2):40-54]
[6] Huang Jin. Geomorphology of Mt. Danxiashan [M]. Beijing:Science Press,2010. [黄进. 丹霞山地貌[M]. 北京:科学出版社,2010.]
[7] Huang Jin. Research report on Danxia Landform in China [J]. Tropical Geography,1992,12(Suppl.):1-36 [黄进. 中国丹霞地貌研究汇报[J]. 热带地理,1992,12(增刊):1-36]
[8] Peng Hua. The red stone park of China——Danxiashan [M]. Beijing:Geological Publishing House,2004. [彭华. 中国红石公园——丹霞山[M]. 北京:地质出版社,2004.]
[9] Peng Hua. Research on landscape geomorphology in Danxiashan [J]. Tropical Geography,1992,12(Suppl.):66-76 [彭华. 丹霞山风景地貌研究[J]. 热带地理,1992,12(增刊):66-76]
[10] Zhu C,Peng H,Ouyang J,et al. Rock resistance and the development of horizontal grooves on Danxia slopes [J]. Geomorphology. 2010,123:84-96
[11] Zhu C,Peng H,Li Z X ,et al. Age and genesis of the Danxia landform on Jianglang Mountain,Zhejiang Province [J]. Journal of Geographical Sciences,2009,19:615-630
[12] Zhu Cheng,Peng Hua,Ouyang Jie,et al. Age genesis and characteristics of Danxia landform of Fangyan in Zhejiang Province,China [J]. Scientia Geographica Sinica,2009,29(2):229-237[朱诚,彭华,欧阳杰,等. 浙江方岩丹霞地貌发育的年代、成因与特色研究[J]. 地理科学,2009,29(2):229-237]
[13] Jon Boxerman. Tafoni[EB/OL]. 2012. http://tafoni.com
[14] Penck D A. Morphologie der Erdoberflche [M]. Stuttgart:Verlag von J. Engelhorn,1894.
[15] Soukis K,Koufosotiri E,Stournaras G. Special landforms on Tinos Island:spheroidal weathering “TAFONI“ forms [G]//Mytilini:3rd International Scientific Symposium of Protected areas and Natural Monuments,1998. (In Greek)
[16] Evelpidou N,Leonidopoulou D,Vassilopoulos A. Tafoni and Alveole formation. An example from Naxos and Tinos islands [G]//Evelpidou N,Figueiredo T,Mauro F et al. Natural Heritage from East to West. Heidelberg:Springer-Verlag,2010. 35-42
[17] Chen Guoda. One explanation for the geomophogensis of white spot in red bed [J]. Geological Review,1941,6(Z3):393-396 [陈国达. 红色岩层中白点成因一解[J]. 地质评论,1941,6(Z3):393-396]
[18] Bureau of Geology of Foshan City,706 Geological Team of Bureau of Geology of Guangdong Province. Geological genesis of Danxia Landform in Mt. Danxiashan Global Geopark [R]. Foshan:Bureau of Geology of Foshan City in Guangdong,2008. [广东省佛山地质局,广东省地质勘查局七〇六地质大队. 丹霞山世界地质公园丹霞地貌地质成因研究[R]. 佛山:广东省佛山地质局,2008.]
[19] Theodoropoulos D. Honeycomb weathering phenomena (TAFONI) on Tinos Island [J]. Annales Géol. des pays Hellén,1975,XXVI:149-158
[20] Ewald H. A pictorial study of tafoni development from the 2nd millennium BC [J]. Geomorphology,2005,64:87-95
[21] Dana J D. Manual of Geology,1st ed [M]. Ivison,Blakeman,Taylor and Company,New York. 1849.
[22] Schaffer R J. The Weathering of Natural Building Stones [M]. Garston (reprinted 1972),1932:149
[23] McGreevy J P. Thermal properties as controls on rock surface temperature maxima and possible implications for rock weathering [J]. Earth Surf. Process. Landf. 1985(10):125–136
[24] Sancho C,Benito G.. Factors controlling tafoni weathering in the Ebro Basin (NE Spain) [J]. Z. Geomorphol. 1990,34(2),165–177
[25] Paradise T R. Sandstone weathering and aspect in Petra,Jordan [J]. Z. Geomorphol. 2002(46):1-17
[26] Paradise T R. Assessment of tafoni distribution and environmental factors on a sandstone djinn block above Petra,Jordan [J]. Applied Geography,2013(42):176-185
[27] Blackwelder E. The insolation hypothesis of rock weathering [J]. Am. J. Sci. 1933(21):140-144
[28] Griggs D T. The factor of fatigue in rock exfoliation [J]. J. Geol. 1936(9):783-796
[29] Robinson D A. Williams,R.B.G.,Experimental weathering of sandstone by combinations of salts [J]. Earth Surf. Process. Landf. 2000(25):1309-1315
[30] Wellman H W,Wilson A T. Salt weathering,a neglected geological erosive agent in coastal and arid environments [J]. Nature,1965,205:1097-1098
[31] Evans I S. Salt crystallisation and rock weathering:a review [J]. Revue de Géomorphologie Dynamique,1970,19(4):153-177
[32] Bradley W C,Hutton J T,Twidale C R. Role of salts in development of granitic tafoni,South Australia [J]. J. Geol.,1978,86:647-654
[33] Kamh G M E. Weathering at high latitudes on the Carboniferous Old Red Sandstone,petrographic and geotechnical investigations,Jedburgh Abbey Church,Scotland,a case study [J]. Environmental Geology,2005,47(4):482-492
[34] Qu Jianjun,Zhang Weimin,Wen Zixiang et al. Environmental geological hazards in Mogao Grotto area of Dunhuang [J]. Marine Geology & Quaternary Geology,1995,15(3):113-119. [屈建军,张伟民,文子祥, 等. 论敦煌莫高窟的环境地质灾害[J]. 海洋地质与第四纪地质,1995,15(3):113-119]
[35] Doehne E. Salt weathering:a selective review [M]. Geological Society,London,Special Publications,2002,205:51-64
[36] Mellor A,Short J,Kirkby S J. Tafoni in the El Chorro area,Andalucia,Southern Spain [J]. Earth Surface Processes and Landforms,1997,22:817-833
[37] Matsuoka N. Rock weathering processes and landform development in the Sr Rondane Mountains,Antarctica [J]. Geomorphology,1995,12:323-339
[38] Turkington A V,Paradise T R. Sandstone weathering:a century of research and innovation [J]. Geomorphology,2005,67:229-253
[39] Dragovich D. Cavern microclimates in relation to preservation of rock art [J]. Stud. Conserv. 1981(26):143-149
[40] Turkington A V,Smith B J,Basheer P A M. The effect of block retreat on subsurface temperature and moisture conditions in sandstone [G]//Prikryl,R.,Viles,H. (Eds.),Understanding and Managing Stone Decay. Prague:Karolinum Press,2002:113-126
[41] Wilhelmy H. Klimamorphologie der Massengesteine [M]. Braunschweig:Georg Westermann Verlag,1958.
[42] Riedl,H. Beitrge zur regionalen Geographie der Insel Tinos (Kykladen) mit besonderer Berücksichtigung des quasinatürlichen Formenschatzes [M]. Beitrge zur Landeskunde von Griechenland V,Band 29,Salzburger Geographische Arbeiten. Salzburg.1995.
[43] Benito M I,Horra R,Barrenchea,J F et al. Late Permian continental sediments in the SE Iberian Ranges,eastern Spain:Petrological and mineralogical characteristics and palaeoenvironmental significance[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,2005,229:24-39
[44] Michèle van Panhuys-Sigler,Nigel H. Trewin,John Still. Roscoelite associated with reduction spots in Devonian red beds,Gamrie Bay,Banffshire [J]. Scottish Journal of Geology,1996,32:127-132
[45] Weibel R,Friis H. Opaque minerals as keys for distinguishing oxidising and reducing diagenetic conditions in the Lower Triassic Bunter Sandstone,North German Basin [J]. Sedimentary Geology,2004,169:129-149
[46] Weibel R. Diagenesis in oxidising and locally reducing conditions—an example from the Triassic Skagerrak Formation,Denmark [J]. Sedimentary Geology,1998,121:259-276
[47] Stel H. Diagenetic crystallization and oxidation of siderite in red bed (Buntsandstein) sediments from the Central Iberian Chain,Spain [J]. Sedimentary Geology,2009,213:89-96
[48] Nakamura N,Borradaile G. Do reduction spots predate finite strain? A magnetic diagnosis of Cambrian slates in North Wales [J]. Tectonophysics,2001,340:133-139
[49] Mykura H,Hampton B P. On the mechanism of formation of reduction spots in the Carboniferous/Permian red beds of Warwickshire [J]. Geol. Mag,1984,121(1):71-74

备注/Memo

备注/Memo:
收稿日期(Received date):2014-04-12;改回日期(Accepted):2014-05-04。
基金项目(Foundation item):国家自然科学
基金项目(41371204,41171163);国家科技基础性专项重点项目(2013FY111900)。[National Natural Science Foundation of China(41371204, 41171163);National science and technology basic special key projects(2013FY111900).]
作者简介(Biography):谭艳(1990-),女,宁夏石嘴山人,硕士研究生,主要研究方向为地貌与第四纪环境演变。[Tan Yan(1990-), female, born in Shizuishan of Ningxia, postgraduate student, in Geomorphology and quaternary environmental change analysis. ] E-mail: tanyan9001@126.com *
通信作者(Corresponding author):朱诚[Zhu Cheng],E-mail: zhuchengnj@126.com;吴立[Wu Li],E-mail: jedi-wuli@163.com
更新日期/Last Update: 1900-01-01