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Record #119443:

Cenozoic glacial history of the Ross Sea revealed by intermediate resolution seismic reflection data combined with drill site information / John B. Anderson, Louis Robert Bartek.

Title: Cenozoic glacial history of the Ross Sea revealed by intermediate resolution seismic reflection data combined with drill site information / John B. Anderson, Louis Robert Bartek.
Author(s): Anderson, John B.
Bartek, Louis Robert.
Date: 1992.
In: Antarctic Research Series. (1992.), Vol. 56 (1992)
Abstract: Detailed record of ice-sheet grounding episodes on Ross Sea continental shelf. Most dramatic evidence of glacial erosion and deposition began in Early Miocene, when troughs as large as those of modern ice sheet were carved. Increased frequency of grounding is believed to have been in response to higher frequency eustatic changes caused by expansion or contraction of northern-hemisphere ice sheets and, possibly, east Antarctic ice sheet. All seismic unite recognized here can be sampled by shallow drilling when coupled with seismic data.
Notes:

Antarctic Research Series. Vol. 56 :231-263 (1992).

Keywords: 551.336 -- Ice ages.
551.77 -- Cenozoic.
551.337 -- Chronology of the Pleistocene and recent periods.
551.33 -- Glacial geology.
551.331 -- Glacial erosion.
551.332 -- Glacial deposition.
E7 -- Glaciology: glacial geology and ice ages.
(*7) -- Antarctic regions.
(*80) -- Southern Ocean.
(*881) -- Ross Sea.
SPRI record no.: 119443

MARCXML

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100 1# ‡aAnderson, John B.
245 10 ‡aCenozoic glacial history of the Ross Sea revealed by intermediate resolution seismic reflection data combined with drill site information /‡cJohn B. Anderson, Louis Robert Bartek.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 231-263 :‡bill., diag., table, maps.
500 ## ‡aAntarctic Research Series. Vol. 56 :231-263 (1992).
520 3# ‡aDetailed record of ice-sheet grounding episodes on Ross Sea continental shelf. Most dramatic evidence of glacial erosion and deposition began in Early Miocene, when troughs as large as those of modern ice sheet were carved. Increased frequency of grounding is believed to have been in response to higher frequency eustatic changes caused by expansion or contraction of northern-hemisphere ice sheets and, possibly, east Antarctic ice sheet. All seismic unite recognized here can be sampled by shallow drilling when coupled with seismic data.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.77 -- Cenozoic.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.331 -- Glacial erosion.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡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(*881) -- Ross Sea.‡2udc
700 1# ‡aBartek, Louis Robert.
773 0# ‡7nnas ‡tAntarctic Research Series. ‡gVol. 56 (1992) ‡wSPRI-39372
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220924