Zobrazeno 1 - 10
of 159
pro vyhledávání: '"Svecofennian Orogeny"'
Autor:
M. Nironen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 89, Iss 1, Pp 5-19 (2017)
Svecofennian orogen that contain ultramafic rocks. New samples were collected from the picritic and basaltic rocks as well as spatially associated gabbroic rocks, and their major and trace element compositions are presented and discussed here. Althou
Externí odkaz:
https://doaj.org/article/66911576be06416bbf0f57bfb04dc09e
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 86, Iss 1, Pp 41-55 (2014)
The origin of the Vaasa migmatite complex was studied by using whole-rock Sm-Nd and zircon Lu-Hf and U-Pb data in conjunction with whole-rock major and trace element geochemistry. The concordia ages of five Vaasa area granitoid samples are 1.88–1.8
Externí odkaz:
https://doaj.org/article/be374f04b11b4815b44f039282099256
Autor:
N. G. Rizvanova, P. Azimov
Publikováno v:
Petrology. 29:300-314
The mineral assemblage Pl + Bt + Qtz + Grt + Sil + Ilm + Rt ± St (without cordierite) found in metapelites at the Kitela garnet deposit in the North Ladoga Metamorphic Complex, southeastern Fennoscandian Shield, was produced by Barrovian-type (eleva
Publikováno v:
Geologica Acta, Vol 16, Iss 1 (2016)
The earliest Svecofennian magmatism in southern Finland has been dated at 1.90-1.88Ga. As an example of this, the Orijärvi (ca. 1.89Ga) and Enklinge (ca. 1.88Ga) volcanic centres comprise bimodal plutonic batholiths surrounded by volcanic rocks of c
Externí odkaz:
https://doaj.org/article/5df782e4a5f14be496fcc2c8a76aefa5
Autor:
M. Nironen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 83, Iss 1, Pp 5-23 (2011)
Detrital zircon studies suggest that the few quartzite occurrences in southern Finland are younger than 1.87 Ga and express sedimentation after 1.89–1.87 Ga accretional deformation and metamorphism in the Svecofennian orogenic belt. Detailed field
Externí odkaz:
https://doaj.org/article/c50dba3d41f940f9803bca039437df0b
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 77, Iss 2, Pp 105-128 (2005)
U-Pb ages and whole-rock Nd isotope data have been obtained from the Paleoproterozoic lateorogenic migmatizing microcline granites of southwestern Finland. Isotope dilution and ion microprobe U-Pb data on zircons and monazites show that the age spect
Externí odkaz:
https://doaj.org/article/5670b32218ca433d8711d66a06378b45
Pukala intrusion, its age and connection to hydrothermal alteration in Orivesi, southwestern Finland
Autor:
M. Talikka, I. Mänttäri
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 77, Iss 2, Pp 165-180 (2005)
The Pukala intrusion is situated in the Paleoproterozoic Svecofennian domain of the Fennoscandian Shield in the contact region between the Central Finland Granitoid Complex and the Tampere Belt. The acid subvolcanic intrusion, which is in contact or
Externí odkaz:
https://doaj.org/article/4f926ad41ceb47a7b7a35d3e302c0da2
Publikováno v:
Precambrian Research. 324:285-302
Reconstructed variations in stratigraphic thicknesses combined with mapped variations in fold-and-thrust belt structural styles and patterns of the entire Palaeoproterozoic Perapohja Belt in northern Finland show that both the deposition of the 2.4
Autor:
Arkadii A. Kalinin
Publikováno v:
Minerals, Vol 11, Iss 574, p 574 (2021)
Minerals
Volume 11
Issue 6
Minerals
Volume 11
Issue 6
Mineralization of Te and Se was found in gold deposits and uranium occurrences, located in the Paleoproterozoic greenstone belts in Northern Fennoscandia. These deposits are of different genesis, but all of them formed at the late stages of the Sveco