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北极王湾冰海沉积物类型及沉积作用

, PP. 115-123

Keywords: 王湾,冰海沉积物,粒度分析,沉积作用

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Abstract:

王湾作为发育于现代冰盖边缘的开放性峡湾,具有典型的冰海沉积特征,使其成为研究冰海沉积作用的良好场所。对湾内54个表层沉积物进行了粒度分析,并计算了其粒度参数。表层沉积物与其他地区冰碛物、冰水沉积物及冰海沉积物的对比,验证了应用粒度参数散点图在区分冰川亚环境过程中的有效性。参照冰海沉积物划分方案,将王湾的冰海沉积物划分为3类:基本缺乏粉砂和泥的Ⅰ型残副冰碛物、含砂砾的Ⅲ型沉积物和基本缺乏砂砾的Ⅳ型混合副冰碛物。对王湾沉积物的来源和沉积作用作了初步的探讨。

References

[1]  KACZMAREK H,WLODARSKA-KOWALCZUK M,LEGEZYNSKA J,et al.Shallow sublittoral macrozoobenthos in Kongsfjord,West Spitsbergen, Svalbard[J].Polish Polar Research,2005,26(2):137—155.
[2]  HARLAND W B.The definition and identification of tilis and tilites [J].Earth Science,1966,2:225—226.
[3]  ANDERSON J B, KURTZ D D, WEAVER F, et al.Sedimentation on the west Antarctic continental margin[M]//CRADDOCK C.Antarctic Geoscience, Madison Wisconsin: University of Wisconsin press, 1982:1003—1012.
[4]  ELVERH Ii A,LNNE O, SELAND R.Glaciomarine sedimentation in a modern-fjord environment, Spitsbergen[J].Polar Research,1983,1:127—149.
[5]  EYLES C H, EYLES N, MIALL A D.Models of glaciomarine sedimentation and their application to the interpretation of ancient glacial sequences[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 1985, 51: 15—84.
[6]  POWELL R D, MOLNIA B F.Glaciomarine sedimentary processes, facies and morphology of the south-southeast Alaska shelf and fjords[J].Marine Geology, 1989, 85(2-4): 359—390.
[7]  王先兰,梁景周.东南极海域冰海沉积物的类型与特征[J].中国科学:B辑,1990,9:981—989.
[8]  刘耕年,崔之久.南极长城站区松散沉积物的粒度特征及环境意义[J].冰川冻土,1997,19(1):30—37.
[9]  程振波,石学法,吴永华,等.北极地区挪威斯瓦尔巴德群岛及冰川地貌综述[J].海洋科学进展,2008,26(2):260—265.
[10]  SVENDSEN H, BESZCZYNSKA-MLLER A, HAGEN J O, et al.The physical environment of Kongsfjorden Krossfjorden, an arctic fjord system in Svalbard [J].Polar Research,2002,21:133—166.
[11]  ITO H, KUDOH S.Characteristics of water in Kongsfjorden[J].Svalbard.Proc.NIPR Symposium.Polar Meteorology.Glaciology.1997, 11: 211—232.
[12]  FOLK R L,ANDREWS P B,LEWIS D W.Detrital sedimentary rock classification and nomenclature for use in New Zealand [J].New Zealand Journal of Geology and Geophysics,1970,13(4):937—968.
[13]  WENTWORTH C K.A scale of grade and class terms for classics sediments [J].Journal of Geology,1922,30(5):377—392.
[14]  赵东波.常用沉积物粒度分类命名方法探讨[J].海洋地质动态,2009,25(8):40—46.
[15]  成都地质学院陕北队.沉积物(岩)粒度分析及其应用[M].北京:地质出版社,1978: 1—147.
[16]  LANDIM P M, FRAKES L A.Distinction between tills and other diamictons based on textural characteristics[J].Journal of Sedimentary Research, 1968, 38(4): 1213—1223.
[17]  DAHANYAKE K, DASANAYAKE D M.Glacial sediments from Weuda,Sri Lanka [J].Geology, 1981,30: 1—14.
[18]  FOLK R L.A review of grain size parameters [J].Sedimentlogy,1966,6:73—93.
[19]  HAGEN J O,KOHLER J,MELVOLD K,et al.Glaciers in Svalbard: mass balance, runoff and freshwater flux [J].Polar Research,22(2):145—159.
[20]  科尼利厄斯·S小赫尔伯,等.地球科学百科全书[M].张文佑译.伯通出版社,1980: 1—368.
[21]  ANDERSON J B, KURTZ D D, DOMACK E W, et al.Antarctic glacial marine sediments[J].Journal of Geology, 1980, 88: 399—414.
[22]  POWELL R D.A model for sedimentation by tidewater glaciers[J].Annals of Glaciology, 1981, 2: 129—134.
[23]  DOWDESWELL J A. Processes of glaciomarine sedimentation[J].Progress in Physical Geography,1987,11:52—90.
[24]  王先兰.长城湾冰海沉积物成因与来源初探[J].东海海洋,1990,8(4):94—99.
[25]  吴能友,段威武,蔡秋蓉.南极布兰斯菲尔德海峡冰海沉积环境与沉积模式初探[J].南海地质研究,2002,13(1):1—8.
[26]  MATTHEW R B,MICHAEL J H, David H, et al.The landform and sediment assemblage produced by a tidewater glacier surge in Kongsfjorden,Svalbard[J].Quaternary Science Reviews,1999,18:1213—1246.
[27]  HOP H,PEARSON T,HEGSETH E N, et al.The marine ecosystem of Kongsfjorden,Svalbard[J].Polar Research,2002,21:167—208.
[28]  LIPPERT H.Chemical ecology and palatability of marine invertebrates in the sub-arctic Kongsfjord (Spitsbergen)[M]//Ber Polarforsch Meeresforsch 465,2003: 1—118.
[29]  JOZEF WIKTOR B U,TOM MOENS A J.MoensIntertidal meiofauna of a high-latitude glacial arctic fjord (Kongsfjorden, Svalbard) with emphasis on the structure of free-living nematode communities [J].Polar Biology,2005,DOI 10.1007/s00300-005-0022-4.
[30]  中国国家标准化管理委员会.GB/T, 12763.822007海洋调查规范-第8部分:海洋地质地球物理调查[S].北京:中国标准出版社, 2007:1—77.
[31]  赵澄林,朱筱敏.沉积岩石学[M].北京:石油工业出版社,2001: 387—390.
[32]  FRIEDMAN G M.Distinction between dune, beach and river sands form their textural characteristics [J].Journal of Sedimentology and Petrology.1961,31: 1—1223.
[33]  武安斌.冰碛物的粒度参数特征及其与沉积环境的关系[J].冰川冻土,1983,5(2):47—53.
[34]  HAGEN J O, LEFAUCONNIER B. Reconstructed run-of from the high arctic basin Bayelva in Svalbard based on mass balance measurements [J]. Nord Hydrology, 1995, 26: 285—296.
[35]  BOULTON G S,DEYNOUX M(关保德译).冰川环境的沉积作用和古代沉积序列的冰碛与冰碛岩的鉴定[J].地质调查与研究,1982,4.

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