Zobrazeno 1 - 8
of 8
pro vyhledávání: '"G. P. Beakhouse"'
Autor:
G. P. Beakhouse, E C Grunsky, Christopher J.M. Lawley, N ElGoumi, D Yergeau, C Dupuis, V Bécu, Vivien Janvier, Blandine Gourcerol, David A. Schneider, Daniel J. Kontak, P. C. Thurston, Simon E. Jackson, J. F. Gao, Jean Goutier, P Pilote, W Oswald, Benoît Dubé, K Lauzière, Patrick Mercier-Langevin, C.J. Kelly, W Bleeker, Robert A. Creaser, Michel Malo, R J Enkin, A Fontaine, Sébastien Castonguay, Bruno Lafrance, S De Souza, Z. Tóth, A M Beauchamp, Vicki McNicoll, Laura R. Katz, M Pelletier
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fdeb51c8e04a2dfdc0c44a19abafd6b6
https://doi.org/10.4095/296625
https://doi.org/10.4095/296625
Publikováno v:
Economic Geology. 88:1359-1375
Studies of plutonic rocks in Archean terranes such as the southern Abitibi subprovince have been an important component in the development of an accretionary tectonic model for the Superior province. In the southern Abitibi subprovince, pretectonic (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d886451ca04edb275d8abd6401f861d5
https://doi.org/10.2113/gsecongeo.88.6.1359
https://doi.org/10.2113/gsecongeo.88.6.1359
Autor:
G. P. Beakhouse
Publikováno v:
Canadian Journal of Earth Sciences. 14:1481-1489
In the western pan of the Superior province, gneisses and plutonic rocks of the English River subprovince form a 100 km wide, east trending unit bound on both north and south by metavolcanic-granitic subprovinces. Recent investigations have resulted
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b6b63222615e3c2477f9e9ecfae9993
https://doi.org/10.1139/e77-129
https://doi.org/10.1139/e77-129
Autor:
G. P. Beakhouse, P. C. van de Kamp
Publikováno v:
Canadian Journal of Earth Sciences. 16:1753-1763
A 4000 to 7000 m sequence of amphibolite-facies Archean layered gneisses in the Pakwash Lake – Lac Seul area of Northwest Ontario has been examined to determine its origin. The micaceous, relatively fine grained gneisses are concluded to be metased
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32a9144123e99ba8a1fd617b28c3d744
https://doi.org/10.1139/e79-161
https://doi.org/10.1139/e79-161