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Record #110296:
- #110296
Main publication details
MARC recordEffect of Cenozoic ice sheet fluctuations of Antarctica on the stratigraphic signature of the Neogene / Louis Robert Bartek, P.R. Vail, James B. Anderson, P.A. Emmet, S. Wu.
| Title: | Effect of Cenozoic ice sheet fluctuations of Antarctica on the stratigraphic signature of the Neogene / Louis Robert Bartek, P.R. Vail, James B. Anderson, P.A. Emmet, S. Wu. |
| Author(s): | Bartek, Louis Robert. Vail, P. R. Anderson, James B. Emmet, P. A. Wu, S. |
| Date: | 1991. |
| In: | Journal of Geophysical Research. (1991.), Vol. 96(B4) (1991) |
| Abstract: | Analysis of worldwide data sets indicates that on continental margins where basin subsidence rates have not changed rapidly, and where there is sufficient sediment supply to prograde into deep water, global Neogene stratigraphic signature is developed. Similarity of Neogene stratal patterns from widely distributed locations to stratal geometry of Ross Sea, Antarctica, suggests that global signature developed in response to glacioeustatic fluctuations. |
| Notes: | Journal of Geophysical Research. Vol. 96(B4) :6753-6778 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.336 -- Ice ages. 551.77 -- Cenozoic. 551.782 -- Neogene. 551.334.4 -- Eustasy, glacial. E7 -- Glaciology: glacial geology and ice ages. (*7) -- Antarctic regions. (*80) -- Southern Ocean. (*826) -- Weddell Sea. |
| SPRI record no.: | 110296 |
LDR 01606naa#a2200000#a#4500 001 SPRI-110296 005 20231208181901.0 007 ta 008 231208s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-110296 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aEffect of Cenozoic ice sheet fluctuations of Antarctica on the stratigraphic signature of the Neogene /‡cLouis Robert Bartek, P.R. Vail, James B. Anderson, P.A. Emmet, S. Wu. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 6753-6778 :‡bdiags., tables, maps. 500 ## ‡aJournal of Geophysical Research. Vol. 96(B4) :6753-6778 (1991). 520 3# ‡aAnalysis of worldwide data sets indicates that on continental margins where basin subsidence rates have not changed rapidly, and where there is sufficient sediment supply to prograde into deep water, global Neogene stratigraphic signature is developed. Similarity of Neogene stratal patterns from widely distributed locations to stratal geometry of Ross Sea, Antarctica, suggests that global signature developed in response to glacioeustatic fluctuations. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.77 -- Cenozoic.‡2udc 650 07 ‡a551.782 -- Neogene.‡2udc 650 07 ‡a551.334.4 -- Eustasy, glacial.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*80) -- Southern Ocean.‡2udc 651 #7 ‡a(*826) -- Weddell Sea.‡2udc 700 1# ‡aBartek, Louis Robert. 700 1# ‡aVail, P. R. 700 1# ‡aAnderson, James B. 700 1# ‡aEmmet, P. A. 700 1# ‡aWu, S. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(B4) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231208