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The High Head Member (Church Point Formation, Goldenville Group, Meguma terrane, Nova Scotia) revisited: new information on relevance for early deep-water colonization
Ayuda Buscar en la ayuda Buscar en la ayuda The High Head Member (Church Point Formation, Goldenville Group, Meguma terrane, Nova Scotia) revisited: new information on relevance for early deep-water colonization Chris E. White [1] ; Sören Jensen [2] ; Sandra M. Barr [1] [1] Acadia University [2] Universidad de Extremadura Localización: Journal of iberian geology: an international publication of earth sciences, ISSN-e 1886-7995, ISSN 1698-6180, Vol. 51, Nº. 3, 2025, págs.
Canadian Science Publishing
Volume 60 • Number 5 • May 2023 Review FREE ACCESS Vol. 60No. 5pp. 464–484 Mount Garibaldi Volcanic System (MGVS) is the southernmost member of Garibaldi Volcanic Belt (GVB), the northern (Canadian) segment of the Cascade Volcanic Arc. Temporally episodic explosive to effusive eruptions may be associated with peak ice unloading after glacial maxima.
Unconformity-bounded rift sequences in Terreneuvian‒Miaolingian strata of the Caledonian Highlands, Atlantic Canada
The Cambrian syn-rift strata preserved in western Avalonia provide a distinctive example of how unconformity-bounded sequences are diachronous throughout proximal to marginal rift branches. Terreneuvian‒Miaolingian third-order sequences of the Caledonian Highlands, New Brunswick, Canada, reflect a complex interplay among syn-rift tectonic events, denudation pulses, and sea-level fluctuations. Unconformably overlying the early, rift-related volcanosedimentary Coldbrook Group (ca.
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