Zobrazeno 1 - 10
of 81
pro vyhledávání: '"O.T. Rämö"'
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 89, Iss 1, Pp 20-34 (2017)
The Salittu Formation is one of the few metavolcanic successions in the U-Pb zircon single grain dating using the LA-MC-ICP-MS technique was utilized to determine the age of the host rocks of the Juomasuo Au-Co-Cu deposit located in the late Archean
Externí odkaz:
https://doaj.org/article/ce47dcf83168446e9ad623b999989d13
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 88, Iss 1, Pp 5-20 (2016)
The Vaasa batholith, western Finland, is a large, peraluminous granitoid pluton that crystallized at 1.88–1.87 Ga during the culmination of the Svecofennian orogeny. The batholith has gradual contacts, through metatexites and diatexites, with the e
Externí odkaz:
https://doaj.org/article/e45ecd9db6c24ef289694a79c58effd5
Autor:
O.T. Rämö, I. Mänttäri
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 87, Iss 1, Pp 25-45 (2015)
Multi-grain isotope dilution and secondary ion microprobe zircon U-Pb as well as wholerock Rb-Sr isotope dilution data on the late Paleoproterozoic Suomenniemi rapakivi granite complex (exposed on the northern flank of the Wiborg batholith in southea
Externí odkaz:
https://doaj.org/article/b59f4b781b9c404a94ae8e2c8232016f
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 86, Iss 2, Pp 71-91 (2014)
The mid-Proterozoic, locus classicus Wiborg rapakivi granite batholith of southeastern Finland and adjacent Russia comprises a varying, bimodal (silicic-basic) sequence of plutonic, subvolcanic, and volcanic rocks. At the current level of erosion sil
Externí odkaz:
https://doaj.org/article/e596b13be1e245628ab3adfd1acdbfed
Autor:
M. Nironen, O.T. Rämö
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 83, Iss 2, Pp 115-122 (2011)
Externí odkaz:
https://doaj.org/article/acf10905519349dcaebe24d509a6156e
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 74, Iss 1-2, Pp 7-52 (2002)
Mineral ages from the A-type granites and anorthosite xenoliths in the Redrock area in the northwestern Burro Mountains in southwestern New Mexico cluster around ~1220–1225 Ma and provide yet another example of bimodal igneous activity during this
Externí odkaz:
https://doaj.org/article/c25dc342d9c84aeca6edfbef06482d34
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
