Zobrazeno 1 - 5
of 5
pro vyhledávání: '"E. W. Domack"'
Autor:
C. Lavoie, E. W. Domack, E. C. Pettit, T. A. Scambos, R. D. Larter, H.-W. Schenke, K. C. Yoo, J. Gutt, J. Wellner, M. Canals, J. B. Anderson, D. Amblas
Publikováno v:
The Cryosphere, Vol 9, Iss 2, Pp 613-629 (2015)
We present a new seafloor map for the northern Antarctic Peninsula (AP), including swath multibeam data sets from five national programs. Our map allows for the examination and interpretation of Last Glacial Maximum (LGM) paleo-ice-flow paths develop
Externí odkaz:
https://doaj.org/article/51abc47cedf24a15a80199ac716d99f4
Autor:
C. Lavoie, E. W. Domack, E. C. Pettit, T. A. Scambos, R. D. Larter, H.-W. Schenke, K. C. Yoo, J. Gutt, J. Wellner, M. Canals, J. B. Anderson, D. Amblas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8fd25c4520a206b460abff97f1aa44e
https://doi.org/10.5194/tcd-8-5321-2014-supplement
https://doi.org/10.5194/tcd-8-5321-2014-supplement
Publikováno v:
Nature. 472:247-247
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2ec7eded138e137b784bdf3b91bfced
https://doi.org/10.1038/nature09931
https://doi.org/10.1038/nature09931
Unconsolidated sediments recovered at Site 740 include approximately 23 m of interbedded siliceous ooze and silty clay (pebbly mud), which was tentatively assigned a late Pliocene to Quaternary age by shipboard scientists. In order to clarify the chr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::465b2807d0cbd15b20f474bf8ef0b6be
https://doi.org/10.2973/odp.proc.sr.119.207.1991
https://doi.org/10.2973/odp.proc.sr.119.207.1991