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Record #84481:
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MARC recordAge dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy / Douglas G. Martinson, Nicklas G. Pisias, James D. Hays, John Imbrie, Theodore C. Moore, Jr., Nicholas J. Shackleton.
| Title: | Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy / Douglas G. Martinson, Nicklas G. Pisias, James D. Hays, John Imbrie, Theodore C. Moore, Jr., Nicholas J. Shackleton. |
| Author(s): | Martinson, Douglas G. Pisias, Nicklas G. Hays, James D. Imbrie, John. Moore, Theodore C., Shackleton, Nicholas J. |
| Date: | 1987. |
| In: | Quaternary Research. (1987.), Vol. 27(1) (1987) |
| Abstract: | Uses stacked oxygen-isotope stratigraphy and four different orbital tuning approaches, each based on different assumption concerning response of orbital signal recorded in data. Differences between chronologies reveal sensitivities of specific tuning techniques and underlying assumptions. Provides basis from which to select and evaluate "best" time scale and degree of convergence helps to answer questions related to orbital/climate link. |
| Notes: | Quaternary Research. Vol. 27(1) :1-29 (1987). |
| Keywords: | 551.337 -- Chronology of the Pleistocene and recent periods. 551.338 -- Ice ages, theories of causation. 550.93 -- Geochronology. E7 -- Glaciology: glacial geology and ice ages. |
| SPRI record no.: | 84481 |
LDR 01542naa#a2200000#a#4500 001 SPRI-84481 005 20230605010032.0 007 ta 008 230605s1987####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-84481 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aAge dating and the orbital theory of the ice ages :‡bdevelopment of a high-resolution 0 to 300,000-year chronostratigraphy /‡cDouglas G. Martinson, Nicklas G. Pisias, James D. Hays, John Imbrie, Theodore C. Moore, Jr., Nicholas J. Shackleton. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 1-29 :‡bdiags., tables. 500 ## ‡aQuaternary Research. Vol. 27(1) :1-29 (1987). 520 3# ‡aUses stacked oxygen-isotope stratigraphy and four different orbital tuning approaches, each based on different assumption concerning response of orbital signal recorded in data. Differences between chronologies reveal sensitivities of specific tuning techniques and underlying assumptions. Provides basis from which to select and evaluate "best" time scale and degree of convergence helps to answer questions related to orbital/climate link. 650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc 650 07 ‡a551.338 -- Ice ages, theories of causation.‡2udc 650 07 ‡a550.93 -- Geochronology.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 700 1# ‡aMartinson, Douglas G. 700 1# ‡aPisias, Nicklas G. 700 1# ‡aHays, James D. 700 1# ‡aImbrie, John. 700 1# ‡aMoore, Theodore C.,‡cJr. 700 1# ‡aShackleton, Nicholas J. 773 0# ‡7nnas ‡tQuaternary Research. ‡gVol. 27(1) (1987) ‡wSPRI-46567 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230605