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Record #109953:
- #109953
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MARC recordIce-3G: a new global model of Late Pleistocene deglaciation based upon geophysical predictions of post-glacial relative sea level change / A. Mark Tushingham, William R. Peltier.
| Title: | Ice-3G: a new global model of Late Pleistocene deglaciation based upon geophysical predictions of post-glacial relative sea level change / A. Mark Tushingham, William R. Peltier. |
| Author(s): | Tushingham, A. Mark. Peltier, William R. |
| Date: | 1991. |
| In: | Journal of Geophysical Research. (1991.), Vol. 96(B3) (1991) |
| Abstract: | New deglaciation model is compared to previous models derived by independent means and tested against additional observations other than sea-level histories, including geologically controlled retreat isochrones, oxygen-isotope data from deep-sea sedimentary cores, and coral terrace elevations. Latter two strongly constrain net sea-level rise that has occurred since onset of deglaciation and therefore mass of ice that melted during last glacial-interglacial transition. |
| Notes: | Journal of Geophysical Research. Vol. 96(B3) :4497-4523 (1991). |
| Keywords: | 519.673 -- Modelling. 551.336 -- Ice ages. 551.791 -- Pleistocene. 551.461.8 -- Palaeo-oceanography. E7 -- Glaciology: glacial geology and ice ages. |
| SPRI record no.: | 109953 |
LDR 01419naa#a2200000#a#4500 001 SPRI-109953 005 20231002055413.0 007 ta 008 231002s1991####xx#b##|##|###|0||#0|eng#d 035 ## ‡aSPRI-109953 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aTushingham, A. Mark. 245 10 ‡aIce-3G :‡ba new global model of Late Pleistocene deglaciation based upon geophysical predictions of post-glacial relative sea level change /‡cA. Mark Tushingham, William R. Peltier. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 4497-4523 :‡btables, maps. 500 ## ‡aJournal of Geophysical Research. Vol. 96(B3) :4497-4523 (1991). 520 3# ‡aNew deglaciation model is compared to previous models derived by independent means and tested against additional observations other than sea-level histories, including geologically controlled retreat isochrones, oxygen-isotope data from deep-sea sedimentary cores, and coral terrace elevations. Latter two strongly constrain net sea-level rise that has occurred since onset of deglaciation and therefore mass of ice that melted during last glacial-interglacial transition. 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.791 -- Pleistocene.‡2udc 650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 700 1# ‡aPeltier, William R. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(B3) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231002