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Watabeag Batholith

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Journal Article
Journal: Economic Geology
Published: 01 October 1993
Economic Geology (1993) 88 (6): 1359–1375.
... characteristics typical of Archean tonalite-trondhjemite suites considered to be derived from melting of basaltic rocks at high metamorphic grades. Late to post-tectonic (<2.69 Ga) diorite-monzonite and syenite plutons (e.g., Watabeag batholith, Lamaque stocks, Otto stock) have large ion lithophile element...
Journal Article
Journal: Economic Geology
Published: 01 October 1993
Economic Geology (1993) 88 (6): 1376–1401.
... partial melting of wet, subducted mafic-ultramafic slabs in a compressional setting.Late tectonic quartz syenite-quartz monzonite-granite batholiths and stocks (the SMG series) were emplaced between 2685 and 2676 Ma in the Abitibi greenstone belt. The Watabeag batholith of this series has a mean delta 18...
Journal Article
Journal: Economic Geology
Published: 01 August 2021
Economic Geology (2021) 116 (5): 1053–1072.
... variation along strike, so it is reasonable to assume that the geology varies most rapidly along the profile and as a function of depth (2-D assumption). However, some features, like batholiths, have a limited strike extent. The software used for the modeling (GM-SYS, see https://www.seequent.com/products...
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Journal Article
Journal: Economic Geology
Published: 01 September 2008
Economic Geology (2008) 103 (6): 1097–1134.
...-trending synclines on the west flank of the Watabeag batholith southeast of Timmins. The presence of an iron formation toward the top of the unit in that area indicates a possible sedimentary interface zone marking a volcanic hiatus of approximately 2 m.y. between the upper part of the Tisdale assemblage...
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Journal Article
Published: 02 April 2000
Canadian Journal of Earth Sciences (2000) 37 (2-3): 135–164.
... in an intraoceanic arc. Late tectonic quartz syenite–quartz monzonite–granite batholiths and stocks (SMG series) were emplaced between 2685 and 2676 Ma. The Watabeag batholith of this series has a mean δ 18 O = 8.2 ± 0.3‰ (1σ). These granites are similar to the TGGM series in overall composition, except...
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Journal Article
Journal: Economic Geology
Published: 01 June 2007
Economic Geology (2007) 102 (4): 537–576.
.../Y = 146
 Yb = 0.38
 La/Yb = 44 2690–2685 7.2 ± 0.5 0.42 ± 0.76
 5.8 ± 3.9 ~2
 ~5 Slab melting and hybridization with mantle wedge Stringer zones of Cu, Pb, Zn, Mo Potassic Rare uneconomic showings, likely magmatic-hydrothermal Late- to post-tectonic SMG Watabeag batholith, Garrison...
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Series: Society of Economic Geologists
Published: 01 January 2017
DOI: 10.5382/Rev.19.01
EISBN: 9781629491172
.... In Ontario, several of these plutons formed in the outcrop area of the Tisdale assemblage between the Porcupine-Destor fault zone in the north and the Larder Lake-Cadillac fault zone in the south ( Fig. 10 ). This includes parts of the Watabeag batholith ( Frarey and Krogh, 1986 ), the Blackstock pluton...
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