Zobrazeno 1 - 10
of 205
pro vyhledávání: '"Lapland Province"'
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 81, Iss 1, Pp 7-38 (2009)
The ~1.8 Ga Nattanen-type granites in the Finnish Lapland and western Kola Peninsula are found as several relatively small, high-level, discordant plutons that are easily discernible as weak maxima on aeromagnetic maps. We present U–Pb mineral isot
Externí odkaz:
https://doaj.org/article/57a4b53f202f4fff8a87435f44bbb4a0
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 79, Iss 2, Pp 143-174 (2007)
Zircons from twelve Palaeoproterozoic granitoids from the Central Lapland Granitoid Complex (CLGC) and from the Hetta Complex (HC) in northern Finland were dated using the NORDSIM ion microprobe. In addition, U-Pb age determinations on zircons from t
Externí odkaz:
https://doaj.org/article/3863ffd52fa9477ea9584b8863b86c1d
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
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 78, Iss 2, Pp 143-175 (2006)
The migmatitic metapelites of the Lapland granulite belt (LGB) in the NE part of the Fennoscandian Shield represent an arc-related greywacke basin metamorphosed in the granulite facies. Detrital zircons from migmatitic metapelites are derived from 1.
Externí odkaz:
https://doaj.org/article/b1b77263775d4b73a7166c1d4482fc04
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 78, Iss 1, Pp 71-105 (2006)
The Palaeoproterozoic Lapland granulite belt was juxtaposed between Archaean and Proterozoic terrains in the NE part of the Fennoscandian Shield concurrently with the accretion of Svecofennian arc complexes at ~1.9 Ga. The belt consists mainly of alu
Externí odkaz:
https://doaj.org/article/ad3e376baf9249eb91e962181364ac3a
Autor:
P. Sarala
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 77, Iss 2, Pp 71-104 (2005)
Quaternary stratigraphy and geomorphology were investigated by using aerial photo interpretation, digital elevation models and stratigraphical studies in southern Finnish Lapland. The development of glacial morphology was examined by reconstructing g
Externí odkaz:
https://doaj.org/article/5df3f2e02eae4e48aaf686963f500619
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 75, Iss 1-2, Pp 69-92 (2003)
The Paleoproterozoic Misi region forms the northeastern part of the Peräpohja Schist Belt in northern Finland. The area comprises mafic volcanic land sedimentary rocks, differentiated gabbros, and late-orogenic granitoids. Three geochemically differ
Externí odkaz:
https://doaj.org/article/ef0b293c630642959abd73dac67bf77f
Autor:
P. Johansson
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 75, Iss 1-2, Pp 5-15 (2003)
Studies of the deglaciation of the last Scandinavian Ice Sheet, including the behavior of the ice sheet and meltwater activity, were conducted in the vicinity of the Pakasaivo canyon lake, located in western Finnish Lapland. Pakasaivo itself, a circu
Externí odkaz:
https://doaj.org/article/aa79faa56bdf4bf38f9de9b07b1519f1
Autor:
M. Nironen, I. Mänttäri
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 75, Iss 1-2, Pp 93-101 (2003)
The Vuotso area is structurally interesting because the fold interference pattern in rocks of central Lapland changes into thrust-related foliation of the Lapland Granulite Belt. A felsic volcanic rock yielded a 2.45 Ga age and conformed that the vol
Externí odkaz:
https://doaj.org/article/ce08327090cc47e0998560a8ba8c277e
Autor:
Hannu Huhma, Laura S. Lauri, Matti Kurhila, Osmo Tapani Rämö, Jaana Halla, K. Front, Esa Heilimo
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 81, Iss 1, Pp 7-38 (2009)
Heilimo, E, Halla, J, Lauri, L S, Rämö, T, Huhma, H, Kurhila, M I & Front, K 2009, ' The Paleoproterozoic Nattanen-type granites in northern Finland and vicinity : A postcollisional oxidized A-type suite ', Bulletin of the Geological Society of Finland, vol. 81, pp. 7-38 . https://doi.org/10.17741/bgsf/81.1.001
Scopus-Elsevier
Heilimo, E, Halla, J, Lauri, L S, Rämö, T, Huhma, H, Kurhila, M I & Front, K 2009, ' The Paleoproterozoic Nattanen-type granites in northern Finland and vicinity : A postcollisional oxidized A-type suite ', Bulletin of the Geological Society of Finland, vol. 81, pp. 7-38 . https://doi.org/10.17741/bgsf/81.1.001
Scopus-Elsevier
The ~1.8 Ga Nattanen-type granites in the Finnish Lapland and western Kola Peninsula are found as several relatively small, high-level, discordant plutons that are easily discernible as weak maxima on aeromagnetic maps. We present U–Pb mineral isot