Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Inge Aarseth"'
Autor:
Eivind Sønstegaard, John Inge Svendsen, Anna L.C. Hughes, Inge Aarseth, Jan Mangerud, Kåre Skår, Øystein S. Lohne
Publikováno v:
Quaternary Science Reviews. 132:175-205
Distinct Younger Dryas (YD) moraines are mapped more-or-less continuously around the Scandinavian Ice Sheet. In most areas there is no evidence to suggest that a glacial re-advance took place during the YD, either because it did not happen or because
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ec5a811cb3639946dd6cb5ff655b381
https://doi.org/10.1016/j.quascirev.2015.11.013
https://doi.org/10.1016/j.quascirev.2015.11.013
Autor:
Haflidi Haflidason, Hans Petter Sejrup, David Long, Inge Aarseth, Edward L. King, Carl Fredrik Forsberg, Kåre Rokoengen
Publikováno v:
Boreas. 23:1-13
Based on new data from the Fladen, Sleipner and Troll areas, combined with earlier published results, a glaciation curve for the Late Weichselian in the northern North Sea is constructed. The youngest date on marine sedimentation prior to the late We
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::abcfecbbdbf6d44a9000b03908dd76fc
https://doi.org/10.1111/j.1502-3885.1994.tb00581.x
https://doi.org/10.1111/j.1502-3885.1994.tb00581.x
Autor:
Jan Mangerud, Inge Aarseth
Publikováno v:
Boreas. 3:3-22
End moraines (called the Herdla Moraines) from the Younger Dryas Stadial arc morphologically mapped along the western coast of Norway, from Hardangerfjorden to north of Sognefjorden. The submarine position of the moraines are found by means of a conv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d26b2ed685e1a3a2df8eb71afc36d7fb
https://doi.org/10.1111/j.1502-3885.1974.tb00663.x
https://doi.org/10.1111/j.1502-3885.1974.tb00663.x
Autor:
Inge Aarseth
Publikováno v:
Naturen. 129:170-178
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a149c6a76930738ab885aeefcc7edb22
https://doi.org/10.18261/issn1504-3118-2005-04-03
https://doi.org/10.18261/issn1504-3118-2005-04-03
Publikováno v:
Marine Geology. 211:45-78
In the last 14–15,000 14 C years BP up to 360 m of sediments were deposited in the 70-km long Ranafjorden, northern Norway. The greatest volume of sediment relates to the Allerod ice recession period, the Younger Dryas ice advance and the succeedin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::043828652ece790c749e720eecf76e81
https://doi.org/10.1016/j.margeo.2004.06.010
https://doi.org/10.1016/j.margeo.2004.06.010
Autor:
Haakon Fossen, Inge Aarseth
Publikováno v:
The Holocene. 14:589-596
A recently discovered lacustrine rock platform at low altitude exists along a 1Okm2 lake on the Osterøy Island near Bergen, western Norway. The lake was converted to a reservoir in 1920 and therefore is subject to frequent changes in level above and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2a463afb1518e7c2fe683caf763ece2
https://doi.org/10.1191/0959683604hl736rp
https://doi.org/10.1191/0959683604hl736rp
Autor:
Inge Aarseth
Publikováno v:
Naturen. 127:99-108
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83191ef34a3cd485ad18c57c16959e9a
https://doi.org/10.18261/issn1504-3118-2003-03-01
https://doi.org/10.18261/issn1504-3118-2003-03-01
Autor:
Inge Aarseth
Publikováno v:
Naturen. 135:188-190
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52e6ed1bf6076ab7b2380bab0b361fbf
https://doi.org/10.18261/issn1504-3118-2011-04-06
https://doi.org/10.18261/issn1504-3118-2011-04-06
Publikováno v:
The Holocene. 11:437-446
A 278 cm long sediment core spanning the last 5500 years was collected from 440 m water depth in Sulafjorden, western Norway. Detailed analyses of benthonic foraminfera, stable isotopes and lithology have been performed on the core, and a chronology
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::221a040a30a44e81750e1c0debbb5201
https://doi.org/10.1191/095968301678302878
https://doi.org/10.1191/095968301678302878
Autor:
Inge Aarseth
Publikováno v:
Marine Geology. 143:39-53
The sediments in the western Norwegian fjords are described chronologically, qualitatively and quantitatively by means of seismic profiling and correlation with dated terrestrial sediments along the fjords. Five chronostratigraphic units (I–V) are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f57e224b8f0a62887f3627d5220e3cc
https://doi.org/10.1016/s0025-3227(97)00089-3
https://doi.org/10.1016/s0025-3227(97)00089-3