Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Greg M. Stott"'
Publikováno v:
Canadian Journal of Earth Sciences. 52:196-214
The greenstone belts along the northern margin of the Wawa subprovince of the Superior Province (Vermilion, Shebandowan, Winston Lake, Manitouwadge) formed at ca. 2720 Ma and have been interpreted to be representative of a rifted-arc to back-arc tect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e799613104a8af85e761e7a3989d09e
https://doi.org/10.1139/cjes-2014-0163
https://doi.org/10.1139/cjes-2014-0163
Publikováno v:
Economic Geology. 109:1291-1313
The ca. 2720 Ma Winston Lake greenstone belt of the Wawa-Abitibi terrane, Superior province, is located on the northern margin of the Wawa subprovince and has important regional tectonostratigraphic implications for the development of the Neoarchean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b156a66b795dd8096bf668854e3ddae8
https://doi.org/10.2113/econgeo.109.5.1291
https://doi.org/10.2113/econgeo.109.5.1291
Autor:
Harold L. Gibson, Michael A. Hamilton, George J Hudak, Robert W.D. Lodge, Mark A. Jirsa, Greg M. Stott
Publikováno v:
Precambrian Research. 235:264-277
Timiskaming-type assemblages in the Wawa–Abitibi terrane of the Superior Craton and other Archean cratons worldwide are important because of their spatial and temporal association with world-class orogenic gold mineralization, especially in the Kir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf4cf04e7c154e6cb40fd2089089206d
https://doi.org/10.1016/j.precamres.2013.06.011
https://doi.org/10.1016/j.precamres.2013.06.011
Publikováno v:
Canadian Journal of Earth Sciences. 44:925-946
The Beardmore–Geraldton belt consists of steeply dipping, intercalated panels of metavolcanic and metasedimentary rocks along the southern margin of the granite–greenstone Wabigoon subprovince in the Archean Superior Province, Ontario. It is an i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4c5edb4db9a5a9cc97c2463deb86c1a
https://doi.org/10.1139/e06-118
https://doi.org/10.1139/e06-118
Autor:
Greg M. Stott, Thomas Skulski, M. Sanborn-Barrie, Don White, Herwart Helmstaedt, John A. Percival
Publikováno v:
Canadian Journal of Earth Sciences. 43:1085-1117
Five discrete accretionary events assembled fragments of continental and oceanic crust into a coherent Superior craton by 2.60 Ga. They exhibit similar sequences of events at 10 million year intervals: cessation of arc magmatism, early deformation, s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c84e744e381f2ef0e3ab28a85ee5565
https://doi.org/10.1139/e06-062
https://doi.org/10.1139/e06-062
Publikováno v:
Precambrian Research. 145:272-288
The Humboldt Bay High Strain Zone (HBHSZ) is the most prominent Archean shear zone within the Onaman-Tashota greenstone belt of the eastern Wabigoon subprovince. The HBHSZ was initiated as a terrane boundary during assembly of the greenstone belt (D1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3bccaa387585ee6b5b6782c4e2b32d86
https://doi.org/10.1016/j.precamres.2005.12.006
https://doi.org/10.1016/j.precamres.2005.12.006
Publikováno v:
Precambrian Research. 132:245-274
The western Superior Province represents a collage of Mesoarchean continental (3.2–2.8 Ga) and Neoarchean continental, arc and oceanic (2.8–2.66 Ga) crustal fragments. Nd isotope data presented here for 89 felsic volcanic and plutonic rocks have
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a995658bd74cf35189d3ce601e6ac315
https://doi.org/10.1016/j.precamres.2003.12.017
https://doi.org/10.1016/j.precamres.2003.12.017
Publikováno v:
Canadian Journal of Earth Sciences. 41:217-235
The BeardmoreGeraldton Belt occurs along the southern margin of the Archean Wabigoon subprovince, Superior Province, Ontario. The belt consists of shear-bounded interleaved metasedimentary and metavolcanic units. The units were imbricated from 2696
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11b0642543764e129d4a53b20e8a4e1e
https://doi.org/10.1139/e03-090
https://doi.org/10.1139/e03-090
Publikováno v:
Scopus-Elsevier
Comprehensive trace element analyses of mafic and felsic volcanic rocks from the 2.85-2.74 Ga Meen-Dempster greenstone belt reveal a wide compositional diversity. The ~2.85 Ga Kaminiskag assemblage is dominated by mafic tholeiite characterized by pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6eba68dbd0c9a29b9b0ab1deda6dd3a9
https://doi.org/10.1139/e00-007
https://doi.org/10.1139/e00-007
Autor:
Wulf Mueller, Greg M. Stott
Publikováno v:
Precambrian Research. 168:1-3
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08e4379538e965adf4da97a5c81c0557
https://doi.org/10.1016/j.precamres.2008.08.008
https://doi.org/10.1016/j.precamres.2008.08.008