Dingle R V,McArthur J M,Vroon P.1997.Oligocene and Pliocene interglacial events in the Antarctic Peninsula dated using strontium isotope stratigraphy.J.Geol.Soc.Lond.,154:257~264.
[8]
Harland W B,Armstrong R L,Cox A V,Craig L E,Smith A G,Smith D G.1990.A Geologic Time Scale 1989.Cambridge Univ.Press,Cambridge,124~125.
[9]
Huang Sijing,Shi He,Shen Licheng,Zhang Meng,Wu Wenhui.2005.Global correlation for strontium isotope curve in the Late Cretaceous of Tibet and dating marine sediments.Science in China (Series D),48(2):199~209 (in English).
[10]
Kaufman A J,Knoll A H,Awramik S M.1992.Biostratigraphic and chemostratigraphic correlation of Neoproterozoic sedimentary successions:Upper Tindir Group,northwestern Canada,as a test case.Geology,20:181~185.
[11]
Korte C,Kozur H W,Bruckschen P,Veizer J.2003.Strontium isotope evolution of Late Permian and Triassic seawater.Geochimica et Cosmochimica Acta,67 (1):47~62.
[12]
McArthur J M,Morton M,Thirlwall M F.2000.Strontium isotope stratigraphy of the Aalenian/Bajocian auxiliary stratotype point at Bearreraig,Isle of Skye,NW Scotland.GeoRes.Forum.,6:137~144.
[13]
Nicora A.1977.Lower Anisian platform-conodonts from the Tethys and Nevada:Taxonomic and stratigraphic revision.Palaeontographica,A157:88~107,Stuttgart.
[14]
Veizer J,Jasper T,Korte C,Schaaf M,Ala D,Azmy K,Buhl D,Diener A,Ebneth S,Podlaha O G,Bruckschen P.1997.Strontium isotope stratigraphy:potential resolution and event correlation.Palaeogeogr.Palaeoclimatol.Palaeoecol.,132:65~77.
[15]
Wickman F E.1948.Isotope ratios:a clue to the age of certain marine sediments.J.Geol.,56:61~66.
[16]
Veizer J,Ala D,Azmy K,Bruckschen P,Buhl D,Bruhn F,Carden G A F,Diener A,Ebneth S,Godderis Y,Jasper T,Korte C,Pawellek F,Podlaha O G.,Strauss H.1999.87Sr/86Sr,δ13C and δ18O evolution of Phanerozoic seawater.Chem.Geol.,161:59~88.
[17]
Walter M R,Veevers J J,Calver C R,Gorjan P,Hill A C.2000.Dating the 840~544 Ma Neoproterozoic interval by isotopes of strontium,carbon,and sulfur in seawater,and some interpretative models.Precambrian Research,100:371~433.
Denison R E,Kirkland D W,Evans R.1998.Using strontium isotopes to determine the age and origin of gypsum and anhydrite beds.J.Geol.,106:1~17.
[27]
Gleason J D,Moore T C,Rea D K,Johnson T M,Owen R M,Blum J D,Hovan S A,Jones C E.2002.Ichthyolith strontium isotope stratigraphy of a Neogene red clay sequence:calibrating eolian dust accumulation rates in the central North Pacific.Earth and Planetary Science Letters,202:625~636.
[28]
Howarth R J,McArthur J M.1997.Statistics for strontium isotope stratigraphy:a robust LOWESS fit to marine Sr-isotope curve for 0 to 206 Ma,with look-up table for derivation of numeric age(look-up table version 8/96).J.Geol.,105:441~456.
[29]
Kaufman A J,Jacobsen S B,Knoll A H.1993.The Vendian record of Sr-and C-isotopic variations in seawater:implications for tectonics and paleoclimate.Earth Planet.Sci.Lett.,120:409~430.
[30]
McArthur J M,Kennedy W J,Chen M,Thirlwall M F,Gale A S.1994.Strontium isotope stratigraphy for the Late Creataceous:direct numerical age calibration of the Sr-isotope curve for the U.S.Western interior Seaway.Palaeogeogr.Palaeoclim.Palaeoecol.,108:95~119.
[31]
McArthur J M,Howarth R J,Bailey T R.2001.Strontium Isotope Stratigraphy:LOWESS Version 3:Best Fit to the Marine Sr-Isotope Curve for 0~509 Ma and Accompanying Look-up Table for Deriving Numerical Age.J.Geol.,109:155~170.
[32]
Melezhik V A,Gorokhov I M,Fallick A E,Gjelle S.2001.Strontium and carbon isotope geochemistry applied to dating of carbonate sedimentation:an example from high-grade rocks of the Norwegian Caledonides.Precambrian Research,108:267~292.
[33]
Price G D,Grcke D R.2002.Strontium-isotope stratigraphy and oxygen-and carbon-isotope variation during the Middle Jurassic-Early Cretaceous of the Falkland Plateau,South Atlantic.Palaeogeogr.Palaeoclimatol.Palaeoecol.,183:209~222.
[34]
Ray J S,Veizer J,Davis W J.2003.C,O,Sr and Pb isotope systematics of carbonate sequences of the Vindhyan Supergroup,India:age,diagenesis,correlations and implications for global events.Precambrian Research,121:103~140.