丹霞地貌是中国地质学家命名的一种地貌类型,国内研究主要在丹霞地貌的理论方面、宏观的空间分布上、以及定性的分类描述上。此外,在丹霞地貌的定量研究、实验研究和可视化研究等方面也有所突破。目前,国外还没有统一使用丹霞地貌这个名词,但在砂岩、砾岩以及红层的微观、实验和定量等方面的研究成果丰富。通过国内外研究的对比,可以使丹霞地貌的研究朝着宏观与微观、定性与定量、理论与实践相结合的方向发展,有利于"丹霞地貌"尽快成为国际认可并接受的地貌名词。
The term "Danxia Landform" was first identified and coined in China. Danxia Landform research in China is focused on primary theoretical research, scientific discussions of macro spatial distribution and qualitative description of the classification. New studies have recently been concerning quantitative,visualization and experimental research for Danxia Landform. Other countries do not currently refer to Danxia Landform as a reference for this unique type of landform very frequently, but foreign scholars have abundant research in sandstones, conglomerates, and red beds in micro, experiments, and quantitative areas. For comparisons with national and international research, Danxia Landforms should be applied as a primary example of macro and micro, qualitative and quantitative, theoretical and practical descriptions and analysis. It is instructive to use the term "Danxia Landform" as an acceptable international term when comparing and contrasting with other like landforms around the world.
[1] Peng H.Danxia Geomorphology of China:A review[J].Chinese Science Bulletin,2001,46 (Supp1):38-44.
[2] Cheng Zhu,Hua Peng,Jie Ouyang,et al.Rock resistance and the development of horizontal grooves on Danxia slopes [J].Geomorphology,2010,123(1-2):84-96.
[3] 彭 华.丹霞地貌分类系统研究[J].经济地理,2002,22(增刊):28~35.
[4] 黄 进.丹霞山地貌[M].北京:科学出版社,2010:227~235.
[5] Zhu C,Peng H,Li Z X,et al.Age and genesis of the Danxia landform on Jianglang Mountain,Zhejiang Province[J].Journal of Geographic Sciences,2009,19(5):615-630.
[6] 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.
[7] Ouyang J, Zhu C, Peng H, et al. Types and spatial combinations of Danxia landform of Fangyan in Zhejiang Province [J]. Journal of Geographic Sciences, 2009, 64 (3):631-640.
[8] Qi D L,Yu R,Zhang R S,et al.On the spatial pattern of Danxia landform in China[J].Acta Geographica Sinica,2005,60 (1):41-52.
[9] 彭 华,蔡 辉.阿切斯-丹霞拱桥大观园[J].经济地理,1998,18(增刊):191~195.
[10] 尹德涛.澳大利亚Uluru-Kata Tjuta丹霞地貌[J].经济地理,2002,22(增刊):235~236.
[11] 张忍顺,齐德利.英国布雷肯毕斯国家公园丹霞景观及旅游开发[J].经济地理,2003,23(增刊):194~199.
[12] Koji U,Kuniyuki F.Timing of remanent magnetization acquisition in red beds:A case study from a syn-folding sedimentary basin[J].Tectonophysics,2005, 406(1-2):67-80.
[13] Harald G D,Obidjan K,Yura T,et al.Palaeogeography of Neogene red bed sequences along the Aksa-Ata River in the Parkent-Nurekata intermontane basin (Tien Shan Mountains,Uzbekistan):With special reference to the magnetic susceptibility of siliciclastic rocks[J].Journal of Asian Earth Sciences,2007,29(5-6):960-977.
[14] Kazuto K,Tetsuichi T.Paleomagnetism of mid-Cretaceous red beds in west-central Kyushu Island,southwest Japan: paleoposition of Cretaceous sedimentary basins along the eastern margin of Asia[J].Earth and Planetary Science Letters,2002,201(1):233-246.
[15] Alice V T,Thomas R P.Sandstone weathering: a century of research and innovation[J].Geomorphology,2005,67(1-2):229-253.
[16] N C Davatzes,A Aydin.Overprinting faulting mechanisms in high porosity sandstones of SE Utah[J].Journal of Structural Geology,2003,25(11):1795-1813.
[17] A Wolela.Diagenetic evolution of the Ansian-Pliensbachian Adigrat Sandstone, Blue Nile Basin[J].Ethiopia,Journal of African Earth Sciences,2010,56 (1):29-42.
[18] Atsushi N,Makoto T,Mamoru A.Provenance of the Murihiku Terrane, New Zealand:evidence from the Jurassic conglomerates and sandstones in Southland[J].Sedimentary Geology,2004,164( 3-4):203-222.
[19] Gérard B,Issa B,Jean J P,et al.Origin and age of Paleoproterozoic conglomerates and sandstones of the Tarkwaian Group in Burkina Faso,West Africa[J].Precambrian Research,1996,80(3-4):153-172.
[20] M Hajpal,A Torok.Mineralogical and colour changes of quartz sandstones by heat Environmental[J].Geology,2004,46:311-322.
[21] G M E Kamh.(A) Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations,Jedburgh Abbey Church,Scotland,a case study[J].Environ Geol,2005,47:482-492.
[22] G M E Kamh.(B) Mechanism of concave ''tafoni’’and convex ''domal shape’’formation on TRIASSIC red sandstone of some old buildings,Chester City,U K,Case study[J].Environ Geol,2005,48:625-638.
[23] Allison R J,Bristow G E.The effects of fire on rock weathering:some further considerations of laboratory experimental simulation[J].Earth Surf Processes Landforms,1999,24:707-713.
[24] Allison R J,Goudie A S.The effects of fire on rock weathering:an experimental study[M]//Robinson D A, Williams RBG (eds).Rock weathering and landform evolution.Wiley:Chichester,1994:41-56.
[25] S McCabe,B J Smith,P A Warke.Preliminary observations on the impact of complex stress Histories on sandstone response to salt weathering:Laboratory simulations of process combinations[J].Environ Geol,2007,52:251-258.
[26] Tony W,Greg H,John F.Weathering rates of sandstone in a semi-arid environment (Hunter Valley,Australia)[J].Environ Geol,2008,54:1047-1057.
[27] Sergei S,Jerom F,Yves G,et al.Initiation and Propagation of Compaction Bands in Dry and Wet Bentheim Sandstone[J].Pure appl.Geophys,2009,166:843-868.
[28] Kinji M.Identification of Sandstone Body Types by Computer Method[J].Mathematical Geology,1979,11(3):269-283.
[29] Robert Schoner,Reinhard Gaupp.Contrasting red bed diagenesis: the southern and northern marginof the Central European Basin[J].J Earth Sci (Geol Rundsch),2005,94:897-916.
[30] Alexandre R C,Georges B,Bruce E T.The Transfiguration continental red-bed Cu-Pb-Zn-Ag deposit,Quebec Appalachians[J].Canada, Miner Deposit,2009,44:285-301.
