Martinson age dating and the orbital theory Cam2cam random gratis

The resultant chronology is also insensitive to the specific indicator used.

The error associated with each tuning approach is estimated independently and propagated through to the average result.

Quaternary Research, 27, 1-29Using the concept of 'orbital tuning', a continuous, high-resolution deep-sea chronostratigraphy has been developed spanning the last 300,000 yr.

Age dating and isotopic analyses of sediment core RC11-120, supplementary data to: Martinson, Douglas G; Pisias, Nicklas G; Hays, James D; Imbrie, John D; Moore, Theodore C; Shackleton, Nicholas J (1987): Age Dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy.

Quaternary Research, 27, 1-29Age dating and isotopic analyses of sediment core RC11-120, supplementary data to: Martinson, Douglas G; Pisias, Nicklas G; Hays, James D; Imbrie, John D; Moore, Theodore C; Shackleton, Nicholas J (1987): Age Dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy.1968: Kominz ands Pisias, 1979; Ruddiman and Mc Intyre,s1979: Imbrie and Imbrie, 1980) agree withs Milankovitch that the high northern lati-stude during summer months i...Citation Context ..significance of thesesparameters, or “paleoclimatic indicators,”sis uncertain (Shackleton 1977; Broecker,s1982; Shackleton and Opdyke, 1973; Haysset al., 1976; Imbrie and Kipp, 1971; Berger,s1973; =-=Dunn, 1982-=-; Moore et al., 1982). Citation Context ..despite a couple of ob-svious miscorrelations resulting from theslarge, relative-amplitude discrepancies be-stween the data and tuning target which co-sincide with an apparent hiatus in the datas(=-=Martinson, 1982-=-, p. Smaller miscor-srelations result from the difference in char-sacter between the data and irradiationscurve.Re-sgardless, despite differences in the char-sacter of the individual records, they all dis-splay some similarities in the timing of cer-stain peaks and troughs (Fig. Using the concept of “orbital tuning, ” a continuous, high-resolution deep-sea chronostra-tigraphy has been developed spanning the last 300,000 yr.

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