[1] Rubinson,M,Clayton,N.Carbon 13 fractionation between aragonite and calcite.Geochim.Cosmochim.Acta,1969,33,997.
[2] Stuiver,M.Oxygen and carbonisotope ratios of fresh-water carbonates as climatic indicators.J.Geophy.Res.,1970,75,5247-5257.
[3] Bowen,R.Isotopes and Climates.Elsevier Applied Science,1990.96-100.
[4] Savin,S.The history of the Earth’s surface temperature during the past 100 million years.Ann.Rev.Earth Planet.Sci., 1977,5,319-335.
[5] Burcharott,B.,Fritz,P.Environmental isotopes as environmental and climatological indicators,in:Handbook of Environmental Isotope Geochemistry,Part I.eds P.Fritz and J.C.Fontes.Elsevier Scientific Publishers,Amsterdam,1980. 478-504.
[6] Abell,P.Oxygen isotope ratios in modern African gastropod shells:a data base for paleoclimalogy.Chem.Geol.,Isotope Geosci.,1985,58,183-193.
[7] 吴敬禄,王苏民.青藏高原东部RM孔碳酸盐同位素揭示的末次间冰期气候特征,科学通报,1996,41(17):(1601-1604).
[8] Mook,W.Carbon 13 in hygrogeological studies.in:Handbook of Environment al Isotope Geochemistry,Part I.eds P. Fritz and J.C.Fontes.Elsevier Scientific Publishers,Amsterdam,1980.49-47.
[9] Emrich,k.et al.Carbon isotope fractionation during the precipitation of calcium carbonate.Earth Planet.Sci.Letts., 1970,8,363-371.
[10] Rubinson,M.,Clayt on,R.N.Carbon 13 fraction between aragonite and calcite.G eochim.Cosmochim.Acta,1969, 33,997-1002.
[11] GRIP members,Climate instability during the last interglacial period recorded in the GRIPice core,Nature,1993.364, 203-207.
[12] 王云飞,王苏民,薛滨,等.黄河袭夺若尔盖古湖时代的沉积学依据.科学通报,1995,40(8):723-725. |