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- W2316422016 abstract "s – GAC Newfoundland Section, 2007 Spring Technical Meeting Atlantic Geology, 2007, Volume 43, Number 1 Copyright © 2015 Atlantic Geology atlantic geology . volume 43 . 2007 82 Copyright © Atlantic Geology, 2007 Gander block (St. Croix) docked, causing proximal turbidite deposition (Vassalboro, southeastern margin of CM) and distal anoxia (Smalls Falls) in the former forearc. Slab break-off triggered minor within-plate volcanism. The Acadian foreland system, prominent in Maine, propagated northwestward following the docking of Avalon. Two examples from Maine illustrate how Appalachian tectonics may contribute to a general understanding of tectonicclimate linkages. First, Penobscot orogeny and the emergence of the New Caledonian ophiolite share much in common. The latter event coincided with the onset of Antarctic glaciation at 34 Ma. In both cases, the exhumation of soluble basic and ultrabasic rocks caused sequestering of atmospheric carbon dioxide through silicate weathering and organic carbon burial. For the 34 Ma event, a rapid trigger is needed to explain the climatic overshoot, and slab breakoff seems a plausible candidate. Second, near Farmington, a recently discovered slumped horizon rests directly on black shales, suggesting a methane release trigger for the slump. This relationship resembles the mechanism invoked for terminal Paleocene extinction, the best ancient analog for the worst-case future global warming scenario. Abstracts – GAC Newfoundland Section, 2007 Spring Technical Meetings – GAC Newfoundland Section, 2007 Spring Technical Meeting" @default.
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- W2316422016 date "2007-01-01" @default.
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- W2316422016 title "Abstract: A maritime perspective on Maine’s Gander Zone, including a few thoughts on tectonic-climate linkages" @default.
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