The Sverdrup Basin Magmatic Province is a large igneous province located on Axel Heiberg Island and Ellesmere Island, Nunavut, Canada near the rifted margin of the Arctic Ocean at the end of Alpha Ridge.[1]
With an area of 550,110 km2, the Sverdrup Basin Magmatic Province forms part of the larger High Arctic Large Igneous Province[2][3] and consists of flood basalts, dikes and sills[4] which form two volcanic formations called the Ellesmere Island Volcanics and Strand Fiord Formation.
The flood basalt lava flows are similar to those of the Columbia River Basalt Group in the U.S. states of Washington, Oregon and Idaho.
See also
editReferences
edit- ^ Robert Meneley (2008). "The Significance of Oil in the Sverdrup Basin" (PDF). Archived from the original (PDF) on 2011-07-19. Retrieved 2010-06-30.
- ^ Bédard, Jean H; Troll, Valentin R; Deegan, Frances M; Tegner, Christian; Saumur, Benoit M; Evenchick, Carol A; Grasby, Stephen E; Dewing, Keith (2021-06-09). "High Arctic Large Igneous Province Alkaline Rocks in Canada: Evidence for Multiple Mantle Components". Journal of Petrology. 62 (egab042). doi:10.1093/petrology/egab042. ISSN 0022-3530.
- ^ Bédard, Jean H; Saumur, Benoît-Michel; Tegner, Christian; Troll, Valentin R; Deegan, Frances M; Evenchick, Carol A; Grasby, Stephen E; Dewing, Keith (2021-06-09). "Geochemical systematics of High Arctic Large Igneous Province continental tholeiites from Canada – Evidence for progressive crustal contamination in the plumbing system". Journal of Petrology. 62 (egab041). doi:10.1093/petrology/egab041. ISSN 0022-3530.
- ^ Deegan, F.M.; Troll, V.R.; Bédard, J.H.; Evenchick, C.A.; Dewing, K.; Grasby, S.; Geiger, H.; Freda, C.; Misiti, V.; Mollo, S. (May 2016). "The stiff upper LIP: investigating the High Arctic Large Igneous Province". Geology Today. 32 (3): 92–98. doi:10.1111/gto.12138. S2CID 130366151.
- Igneous, metamorphic and volcanic studies[permanent dead link]
- Flood basalts of the Sverdrup Basin Magmatic Province, Canadian Arctic Islands, Nunavut: an overview[permanent dead link]
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