Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises
The Amundsen Sea embayment lies between the Palaeozoic crustal blocks of Marie Byrd Land, Ellsworth Land and Thurston Island. Its continental margin is conjugate to the passive margin of the eastern New Zealand submarine continental plateaux and Bounty Trough, which underwent major extension during...
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ftawi:oai:epic.awi.de:17108 2024-09-15T17:38:58+00:00 Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises Gohl, Karsten Larter, R. D. Eagles, G. Uenzelmann-Neben, Gabriele Kuhn, Gerhard Hillenbrand, C. D. Deen, T. Nitsche, F. 2006 https://epic.awi.de/id/eprint/17108/ https://hdl.handle.net/10013/epic.26961 unknown Gohl, K. orcid:0000-0002-9558-2116 , Larter, R. D. , Eagles, G. , Uenzelmann-Neben, G. orcid:0000-0002-0115-5923 , Kuhn, G. orcid:0000-0001-6069-7485 , Hillenbrand, C. D. , Deen, T. and Nitsche, F. (2006) Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises , 13th Annual West Antarctic Ice-Sheet (WAIS) Workshop, 27-30 Sept., Pack Forest Conference Center, Eatonville, WA, USA. . hdl:10013/epic.26961 EPIC313th Annual West Antarctic Ice-Sheet (WAIS) Workshop, 27-30 Sept., Pack Forest Conference Center, Eatonville, WA, USA. Conference notRev 2006 ftawi 2024-06-24T03:59:51Z The Amundsen Sea embayment lies between the Palaeozoic crustal blocks of Marie Byrd Land, Ellsworth Land and Thurston Island. Its continental margin is conjugate to the passive margin of the eastern New Zealand submarine continental plateaux and Bounty Trough, which underwent major extension during Cretaceous rifting between New Zealand and West Antarctica. Later, the embayment seems to have played a role as a plate boundary while the Bellingshausen Plate acted as an independent microplate until the early Tertiary. It is likely that the tectonic architecture, through the formation of deep basins and erosional troughs, laid the foundation for major glacier outflow from the West Antarctic Ice Sheet into Pine Island Bay and the South Pacific since early West Antarctic glaciation.During successive cruises on RRS James Clark Ross (cruise JR141) and RV Polarstern (expedition ANT-XXIII/4) in early 2006, we collected seismic, bathymetric, sub-bottom profiler and helicopter-magnetic data from the inner shelf, outer shelf, slope and deep sea of the Amundsen Sea embayment and Pine Island Bay, to address tectonic as well as sedimentary objectives. We will present preliminary results indicating the disposition of structural basement units and the role the tectonic basement and pre-glacial sediments have played as controlling parameters for ice-sheet expansion and retreat in the Amundsen Sea Embayment. Conference Object Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet Marie Byrd Land Pine Island Pine Island Bay Thurston Island West Antarctica Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
The Amundsen Sea embayment lies between the Palaeozoic crustal blocks of Marie Byrd Land, Ellsworth Land and Thurston Island. Its continental margin is conjugate to the passive margin of the eastern New Zealand submarine continental plateaux and Bounty Trough, which underwent major extension during Cretaceous rifting between New Zealand and West Antarctica. Later, the embayment seems to have played a role as a plate boundary while the Bellingshausen Plate acted as an independent microplate until the early Tertiary. It is likely that the tectonic architecture, through the formation of deep basins and erosional troughs, laid the foundation for major glacier outflow from the West Antarctic Ice Sheet into Pine Island Bay and the South Pacific since early West Antarctic glaciation.During successive cruises on RRS James Clark Ross (cruise JR141) and RV Polarstern (expedition ANT-XXIII/4) in early 2006, we collected seismic, bathymetric, sub-bottom profiler and helicopter-magnetic data from the inner shelf, outer shelf, slope and deep sea of the Amundsen Sea embayment and Pine Island Bay, to address tectonic as well as sedimentary objectives. We will present preliminary results indicating the disposition of structural basement units and the role the tectonic basement and pre-glacial sediments have played as controlling parameters for ice-sheet expansion and retreat in the Amundsen Sea Embayment. |
format |
Conference Object |
author |
Gohl, Karsten Larter, R. D. Eagles, G. Uenzelmann-Neben, Gabriele Kuhn, Gerhard Hillenbrand, C. D. Deen, T. Nitsche, F. |
spellingShingle |
Gohl, Karsten Larter, R. D. Eagles, G. Uenzelmann-Neben, Gabriele Kuhn, Gerhard Hillenbrand, C. D. Deen, T. Nitsche, F. Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises |
author_facet |
Gohl, Karsten Larter, R. D. Eagles, G. Uenzelmann-Neben, Gabriele Kuhn, Gerhard Hillenbrand, C. D. Deen, T. Nitsche, F. |
author_sort |
Gohl, Karsten |
title |
Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises |
title_short |
Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises |
title_full |
Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises |
title_fullStr |
Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises |
title_full_unstemmed |
Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises |
title_sort |
basement control and history of ice-sheet expansion in the amundsen sea embayment - first results of recent rv polarstern and rrs james clark ross cruises |
publishDate |
2006 |
url |
https://epic.awi.de/id/eprint/17108/ https://hdl.handle.net/10013/epic.26961 |
genre |
Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet Marie Byrd Land Pine Island Pine Island Bay Thurston Island West Antarctica |
genre_facet |
Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet Marie Byrd Land Pine Island Pine Island Bay Thurston Island West Antarctica |
op_source |
EPIC313th Annual West Antarctic Ice-Sheet (WAIS) Workshop, 27-30 Sept., Pack Forest Conference Center, Eatonville, WA, USA. |
op_relation |
Gohl, K. orcid:0000-0002-9558-2116 , Larter, R. D. , Eagles, G. , Uenzelmann-Neben, G. orcid:0000-0002-0115-5923 , Kuhn, G. orcid:0000-0001-6069-7485 , Hillenbrand, C. D. , Deen, T. and Nitsche, F. (2006) Basement control and history of ice-sheet expansion in the Amundsen Sea Embayment - First results of recent RV Polarstern and RRS James Clark Ross cruises , 13th Annual West Antarctic Ice-Sheet (WAIS) Workshop, 27-30 Sept., Pack Forest Conference Center, Eatonville, WA, USA. . hdl:10013/epic.26961 |
_version_ |
1810476464442703872 |