Zobrazeno 1 - 10
of 37
pro vyhledávání: '"M. Poutiainen"'
Autor:
S. Frindt, M. Poutiainen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 74, Iss 1-2, Pp 103-114 (2002)
The Gross Spitzkoppe granite stock (GSS) is a zoned 30 km2 epizonal intrusion that consists of three main granites: 1) medium-grained biotite granite (marginal), 2) a coarse-grained biotite granite, and 3) a central, porphyritic granite. The stock co
Externí odkaz:
https://doaj.org/article/63c2caeb017c4bc1aa1057232d679b39
Autor:
M. Pajunen, M. Poutiainen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 71, Iss 1, Pp 73-132 (1999)
Several occurrences of coarse-grained kyanite rocks are exposed in the Archaean area of eastern Finland in zones trending predominantly northwest-southeast that crosscut all the Archaean structures and, locally, the Palaeoproterozoic metadiabase dyke
Externí odkaz:
https://doaj.org/article/ca41137158b3426f902a3dd45525cf77
Autor:
M. Poutiainen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 67, Iss 1, Pp 3-18 (1995)
In the studied zircon and apatite crystals, data recorded two different compositional types of fluid inclusions: Type 1 H2O-CO2 low salinity inclusions (XCO2 = 0.42 to 0.87; XNaCl = 0.001 to 0.005) with bulk densities of 0.73 to 0.87 g/cm3, and Type
Externí odkaz:
https://doaj.org/article/4893f5177be548ab8d3152922f9ebb38
Autor:
M. Poutiainen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 64, Iss 1, Pp 3-12 (1992)
Fluid inclusions both in matrix quartz of metamorphic rocks and in quartz veins from five samples from the Archean high-grade Varpaisjärvi-Lapinlahti area were examined with microthermometric methods. Two types of fluid inclusions were observed: CO2
Externí odkaz:
https://doaj.org/article/dd94d7aff0ed4dc788d4975170c72ca7
Autor:
M. Poutiainen
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 63, Iss 2, Pp 87-93 (1991)
Fluid inclusions in selected cavity quartz crystals in rapakivi granite from Luumäki, southeastern Finland, were studied by microthermometric methods. Two different compositional types of fluid inclusions were identified: (I) low- to intermediate-sa
Externí odkaz:
https://doaj.org/article/596b47e7a8f341b68d6e270f6b86e7cb
Autor:
T.F Scherbakova, M Poutiainen
Publikováno v:
Lithos. 44:141-151
Idiomorphic quartz crystals in topaz-bearing granite from the Salmi batholith contain primary inclusions of silicate melt and abundant mostly secondary aqueous fluid inclusions. Microthermometric measurements on melt inclusions give estimates for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0398e58a84952f678ceee52ced999d9
https://doi.org/10.1016/s0024-4937(98)00052-8
https://doi.org/10.1016/s0024-4937(98)00052-8
Autor:
J. Saltevo, T. Forslund, M. Poutiainen, M. Brummer-Korvenkontio, A. Korhonen, S. Auvinen, J. Anttinen
Publikováno v:
Journal of Internal Medicine. 232:87-90
Haemorrhagic fever with renal syndrome (HFRS) in Scandinavia is called nephropathia epidemica (NE), and is caused by the Puumala-virus, which belongs to the Hanta-virus genus. The clinical course of NE is mostly benign, complications are uncommon, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4b99dbd5e76a4615303879ed6a0cfb48
https://doi.org/10.1111/j.1365-2796.1992.tb00555.x
https://doi.org/10.1111/j.1365-2796.1992.tb00555.x
Autor:
A, Rökman, P A, Koivisto, M P, Matikainen, T, Kuukasjärvi, M, Poutiainen, H J, Helin, R, Karhu, O P, Kallioniemi, J, Schleutker
Publikováno v:
The Prostate. 46(3)
Germline mutations in recessive cancer predisposition genes are uncovered by somatic genetic deletions during tumor development. Analysis of genetic changes in tumor tissues from patients with an inherited predisposition may therefore highlight regio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::0b3a2768db89ea46dccdf231c892b437
https://pubmed.ncbi.nlm.nih.gov/11170152
https://pubmed.ncbi.nlm.nih.gov/11170152
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.