Melting under the Colorado Plateau, USA

Autor: Janne Blichert-Toft, K. Liu, Mary R. Reid, Meghan S. Miller, Frank C. Ramos, Romain A. Bouchet, Alan Levander
Přispěvatelé: School of Earth and Environmental Sustainability, Northern Arizona University [Flagstaff], Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Department of Earth Sciences [Houston], Rice University [Houston], Department of Earth Sciences [USC Los Angeles], University of Southern California (USC), Department of Geological Sciences, New Mexico State University, National Science Foundation (NSF) : EAR-0810274, EAR-1109826, French Institut National des Sciences de l'Univers, NSF EarthScope : EAR-0844741, EAR-0844760, Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Université Grenoble Alpes - UFR Médecine (UGA UFRM), Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Laboratoire de Sciences de la Terre (LST), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon)
Jazyk: angličtina
Rok vydání: 2012
Předmět:
Zdroj: Geology
Geology, Geological Society of America, 2012, 40 (5), pp.387-390. ⟨10.1130/G32619.1⟩
Geology, 2012, 40 (5), pp.387-390. ⟨10.1130/G32619.1⟩
ISSN: 0091-7613
DOI: 10.1130/G32619.1⟩
Popis: International audience; Mafic volcanism gradually encroaching on the tectonically stable Colorado Plateau in the southwestern United States appears to originate from within Paleoproterozoic lithosphere. New Hf and Nd isotope data strengthen evidence for magma source heterogeneity; other geochemical signatures show these sources to consist dominantly of peridotite. Tomographic and receiver function analyses reveal that young volcanism occurs above or outboard of a pronounced shallowing in the lithosphere-asthenosphere boundary. Melt extraction extends to the base of lithosphere thinned to
Databáze: OpenAIRE