Zobrazeno 1 - 10
of 27
pro vyhledávání: '"M. E. Villeneuve"'
Autor:
N Rogers, Gilles Bellefleur, S Paradis, Christopher J.M. Lawley, Simon E. Jackson, Vicki McNicoll, J B Chapman, E G Potter, C Bjerkelund, Jan M. Peter, W J Davis, V Bécu, Patrick Mercier-Langevin, Benoît Dubé, R Evans, M E Villeneuve, Sébastien Castonguay, W Bleeker, Nicolas Pinet, M G Houlé
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::544e209853f3425e385a11e373443928
https://doi.org/10.4095/299574
https://doi.org/10.4095/299574
Autor:
S J Pehrsson, M E Villeneuve
Publikováno v:
Canadian Journal of Earth Sciences. 36:1149-1168
New U-Pb age data from the southwestern Slave Province demonstrate that units of the Indin Lake supracrustal belt form an imbricated structural stack. The oldest rocks of the belt are undated mafic volcanic flows of the Hewitt Lake group that are cro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a7e379b4c257a5da2c523da57eff386
https://doi.org/10.1139/e99-017
https://doi.org/10.1139/e99-017
Publikováno v:
Canadian Journal of Earth Sciences. 36:1207-1226
The Anialik River area in the northwestern Slave Province comprises two geological domains of different age and origin that were tectonically juxtaposed at ca. 2650 Ma. The older domain, the Kangguyak gneiss belt, comprises ca. 3300-2700 Ma orthognei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f72cb74b019d6f87a5739868882d8c8
https://doi.org/10.1139/e99-050
https://doi.org/10.1139/e99-050
Autor:
M. E. Villeneuve, C. Relf
Publikováno v:
Journal of Petrology. 39:1975-1986
lationship between the various intrusive phases of the complex. Finally, the tectonic implications of the complex are addressed, especially with respect to the relationship of carbonatite magmatism to regional tectonic events.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a91400ba06a2be89a6c538c95ed1fa6
https://doi.org/10.1093/petroj/39.11-12.1975
https://doi.org/10.1093/petroj/39.11-12.1975
Publikováno v:
Canadian Journal of Earth Sciences. 28:1003-1008
Two undeformed biotite granites recovered from exploratory hydrocarbon drill holes that penetrated basement in the Fort Simpson magnetic high were analyzed for U–Pb zircon geochronology and Sm–Nd isotopic composition. Both samples give crystalliz
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9969f525f8f3a4a322f71163d5c065cd
https://doi.org/10.1139/e91-091
https://doi.org/10.1139/e91-091
Publikováno v:
Canadian Journal of Earth Sciences. 28:512-522
Although progressively muted by the increasing thickness of Phanerozoic sediments in the Alberta Basin, the geophysical signature of tectonic domains in the Canadian Shield can be traced nearly to the Foothills of the Canadian Cordillera. A combinati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7026b408b710f4382e8249aff43ea5c6
https://doi.org/10.1139/e91-045
https://doi.org/10.1139/e91-045
Autor:
C Lowe, ST Johnson, Michael J. Orchard, R G Anderson, Dante Canil, M Harder, Joseph M. English, K Russell, F Cordey, H Sano, Mitchell G. Mihalynuk, M E Villeneuve
The Atlin Integrated Geoscience Project, jointly funded by federal and provincial governments, entered its third and final year in 2002–2003. It is designed to advance understanding of the geological evolution and mineral potential of the northern
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90949a6e332463588a9314486711d06a
https://doi.org/10.4095/214028
https://doi.org/10.4095/214028
The Yukon–Tanana terrane in the Stewart River area consists of twice-transposed, amphibolite-facies gneiss and schist of mostly of (?)Paleozoic age. Quartz-rich metaclastic rocks (quartzite, quartz-mica schist, psammite, conglomerate) appear to hav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9b813bdb5095cc48e44af2d4be4bd084
https://doi.org/10.4095/214026
https://doi.org/10.4095/214026