Zobrazeno 1 - 10
of 28
pro vyhledávání: '"interglacial environment"'
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 79, Iss 1, Pp 17-39 (2007)
An unusually long and continuous Late Quaternary sedimentary sequence has been preserved in a sedimentary basin formed in the Sokli Carbonatite Massif in eastern-central Finnish Lapland. A nearly complete sediment recovery from the central Sokli basi
Externí odkaz:
https://doaj.org/article/f404f36c92b941819fda0506fddf2439
Autor:
B. Eriksson, R. Kujansuu
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 66, Iss 2, Pp 53-66 (1994)
A till-covered layer of clay, fine sand and organic-bearing silt was found at Hietamäki near Haapajärvi, Ostrobothnia (Pohjanmaa), western Finland. The organic-bearing silt layer is an infill sediment in a dead ice hollow within a glaciofluvial for
Externí odkaz:
https://doaj.org/article/6b8526bad9334d7cbc00d499b066d2a0
Autor:
R. Kujansuu
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 64, Iss 2, Pp 161-167 (1992)
In Ostrobothnia, western Finland, palaeosols have been recognized at several sites in the sandy deposits between glaciofluvial sediments and the overlying till. The palaeosols resemble postglacial podzol. As climatic conditions changed, the palaeosol
Externí odkaz:
https://doaj.org/article/105b0a80a6d142be9f9b674120bf877f
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 64, Iss 2, Pp 169-181 (1992)
More than 100 till-covered organic deposits are currently known in the Finnish Lapland. All others, except Naakenavaara, are interpreted as having deposited during either the Early-Weichselian Peräpohjola/Maaselkä interstadial or the Eemian intergl
Externí odkaz:
https://doaj.org/article/dbea8f27deb94c11ac5e32616aa1969b
Autor:
K. Nenonen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 64, Iss 2, Pp 149-160 (1992)
This paper gives a review over the recent discoveries and results of Quaternary stratigraphical studies in southern and western Finland. The study of Quaternary stratigraphy has been very active and both Quaternary departments in Universities and Geo
Externí odkaz:
https://doaj.org/article/79f2ba51783d479cae1c98a27f5cdb87
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 79, Iss 1, Pp 17-39 (2007)
An unusually long and continuous Late Quaternary sedimentary sequence has been preserved in a sedimentary basin formed in the Sokli Carbonatite Massif in eastern-central Finnish Lapland. A nearly complete sediment recovery from the central Sokli basi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4dff2d9860653f151a8312ca482717a7
https://doi.org/10.17741/bgsf/79.1.002
https://doi.org/10.17741/bgsf/79.1.002
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 64, Iss 2, Pp 169-181 (1992)
More than 100 till-covered organic deposits are currently known in the Finnish Lapland. All others, except Naakenavaara, are interpreted as having deposited during either the Early-Weichselian Peräpohjola/Maaselkä interstadial or the Eemian intergl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::61ec1b95089928b857e73bdee8dfb26d
http://www.geologinenseura.fi/bulletin/Volume64/sgs_bt_064_2_pages_169_181.pdf
http://www.geologinenseura.fi/bulletin/Volume64/sgs_bt_064_2_pages_169_181.pdf
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Akademický článek
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