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N. Wodicka
Researcher at Geological Survey of Canada
Publications - 25
Citations - 976
N. Wodicka is an academic researcher from Geological Survey of Canada. The author has contributed to research in topics: Metamorphism & Craton. The author has an hindex of 14, co-authored 22 publications receiving 870 citations.
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The Palaeoproterozoic Trans-Hudson Orogen: a prototype of modern accretionary processes
TL;DR: The Trans-Hudson Orogen (THO) of North America is one of the earliest orogens in Earth's history that evolved through a complete Wilson Cycle as discussed by the authors.
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Trans-Hudson Orogen of North America and Himalaya-Karakoram-Tibetan Orogen of Asia: Structural and thermal characteristics of the lower and upper plates
TL;DR: In this article, the authors compare the type and duration of tectonothermal events for the Trans-Hudson Orogen and Himalaya-Karakoram-Tibetan Orogen (HKTO) and highlight the complementary nature of the rock record in an older exhumed orogen compared to one undergoing present-day orogenesis.
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Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: Polystage convergence and extension in the lower orogenic crust
Nicholas Culshaw,Rebecca Anne Jamieson,J. W. F. Ketchum,N. Wodicka,David Corrigan,Peter H. Reynolds +5 more
TL;DR: The Grenville orogenic cycle, between ∼ 1190 and 980 Ma, involved accretion of magmatic arcs and/or continental terranes to the Laurentian craton as mentioned in this paper.
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Early Paleoproterozoic supracrustal assemblages of the Rae domain, Nunavut, Canada: Intracratonic basin development during supercontinent break-up and assembly
TL;DR: In this paper, the authors proposed a stratigraphy and detrital zircon geochronology of the Hearne and Rae domains for the Churchill Province in northern Canada.
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Deep crustal ductile extension following thrusting in the southwestern Grenville Province, Ontario
TL;DR: In this paper, the authors postulate that a cryptic Grenvillian thrust separates the assemblages of the two lithotectonic assembls in the southern Britt domain and explain the differences in their histories of plutonism, metamorphism, structural development and mafic dyke emplacement.