Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Kari Strand"'
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 95, Iss 1, Pp 35-46 (2023)
Modern techniques for detrital mineral provenance were applied to sediment core 96/12-1pc from the Lomonosov Ridge in the central Arctic Ocean. The techniques include quantitative clay mineralogy analysis combined with determination of Nd, Pb, and Sr
Externí odkaz:
https://doaj.org/article/7d33ffeac795429d808e0bd80be1cc9a
Publikováno v:
Arctic, Antarctic, and Alpine Research, Vol 54, Iss 1, Pp 624-639 (2022)
ABSTRACTThe Landsort Deep is the deepest part of the Baltic Sea and contains an excellent high-resolution late Pleistocene sediment record suitable to study the retreat history of the southern margin of the Fennoscandian Ice Sheet and the development
Externí odkaz:
https://doaj.org/article/3a13221e4baa4b2988181b96226736b5
Autor:
Eero Hanski, Hannu Huhma, Yann Lahaye, Juha Pekka Lunkka, Erik Nilsson, Timo Mäki, Hugh O´Brien, Kari Strand
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 91, Iss 2, Pp 143-178 (2019)
Over the past tens of years, glacial sandstone erratics variably enriched in Zn, Pb and Cu have been collected from the coast south of Raahe, but their source has remained ambiguous. In these non-metamorphosed and non-deformed boulders, detrital grai
Externí odkaz:
https://doaj.org/article/aaf9a608138e43fb879f6bad99565537
Autor:
Juha Pekka Lunkka, Atle Arctica, Mountain View, Usa, Hannu Huhma, Erik Nilsson, Eero Hanski, Yann Lahaye, Kari Strand, Timo Mäki, Hugh O’Brien
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 91, Iss 2, Pp 143-178 (2019)
Over the past tens of years, glacial sandstone erratics variably enriched in Zn, Pb and Cu have been collected from the coast south of Raahe, but their source has remained ambiguous. In these non-metamorphosed and non-deformed boulders, detrital grai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0fdf059ecbde466a93bed507a825ba56
https://doi.org/10.17741/bgsf/91.2.001
https://doi.org/10.17741/bgsf/91.2.001
The Arctic's glacial history has classically been interpreted from marine records in terms of the fluctuations of the Eurasian and North American ice sheets. However, the existence, size, and timing of the East Siberian Ice Sheet (ESIS) remains highl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c3ce4babc7960d754b62fbe320bee6d
https://doi.org/10.5194/cp-2021-111
https://doi.org/10.5194/cp-2021-111
Autor:
Kari Strand
Publikováno v:
DRAMA. 58:48-49
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db55a4ce2ac80ac6d46f736e01827d34
https://doi.org/10.18261/issn.2535-4310-2021-01-12
https://doi.org/10.18261/issn.2535-4310-2021-01-12
Publikováno v:
Boreas. 47:522-543
Southwestern Barents Sea sediments contain important information on Lateglacial and Holocene environmental development of the area, i.e. sediment provenance characteristics related to ice-flow patterns and ice drifting from different regional sectors
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1895093fa88695a6d460992bc8cc0bff
https://doi.org/10.1111/bor.12293
https://doi.org/10.1111/bor.12293
Publikováno v:
Quaternary Science Reviews. 147:210-220
Mineralogical and geochemical data generated from the well referred shallow core 96/12-1pc on the Lomonosov Ridge, central Arctic Ocean was used to evaluate ice transport from the circum-Arctic sources and variability in sediment drainage and provena
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::68b49d4df77dbe9bf3808a1967b156c3
https://doi.org/10.1016/j.quascirev.2015.09.017
https://doi.org/10.1016/j.quascirev.2015.09.017
Publikováno v:
Quaternary Science Reviews. 92:133-139
Ice-rafted quartz sand grains of sediment samples representing marine isotope stages (MIS) 3 and 4 from the Lomonosov Ridge, Arctic Ocean, are here analysed with a scanning electron microscope (SEM) to characterise processes in the sediment source ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::742276cf9ce3d7468e8ace41e4e9156e
https://doi.org/10.1016/j.quascirev.2014.01.008
https://doi.org/10.1016/j.quascirev.2014.01.008
Autor:
Kari Strand
Publikováno v:
DRAMA. 55:88-88
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eac2ec59abfd191b4c0845e38481d2e3
https://doi.org/10.18261/issn2535-4310-2018-02-03-20
https://doi.org/10.18261/issn2535-4310-2018-02-03-20