Results 41 to 50 of about 196,173 (215)
Metasomatism in oceanic and continental lithospheric mantle: introduction [PDF]
Geological Society, London, Special Publications, 2007 s CD. BODINIER, J.-L., MENZIES, M. A., SHIMIZU, N., FREY, F. A. & MCPHERSON, E. 2004. Silicate, hydrous and carbonate metasomatism at Lherz, France: contemporaneous derivatives of silicate melt–harzburgite reaction. Journal of Petrology, 45, 299–320. BONADIMAN, C., BECCALUVA, L., COLTORTI, M. & SIENA, F. 2005.
COLTORTI, Massimo, Gregoire M.
openaire +2 more sources
, 2017 Mantle-derived eclogite and pyroxenite xenoliths from the Jurassic Voyageur kimberlite on the northern Slave craton in Arctic Canada were studied for garnet and clinopyroxene major and trace element compositions, clinopyroxene Pb and garnet O isotopic ...
K. Smart +5 more
semanticscholar +1 more source
Ambient noise surface wave tomography of marginal seas in east Asia
Earth and Planetary Physics, 2017 We conducted ambient noise tomography in east Asia, including the Chinese coastal provinces, Korea Peninsular, Japan, Taiwan Island, and marginal seas in between.
Qing Wang, XiaoDong Song, JianYe Ren
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The Zagros core: Deformation of the continental lithospheric mantle [PDF]
Geochemistry, Geophysics, Geosystems, 2012 The Zagros of Iran form one of the youngest collisional orogenic belts on Earth. At shallow depths, shortening across the Zagros is accommodated by folding in the sediments, high‐angle thrust faulting in the basement and thickening of the lower crust, but how shortening is accommodated by the lithospheric mantle has been uncertain largely because the ...
Priestley, K. +4 more
openaire +3 more sources
Geological Journal, EarlyView.Early zircon saturation and crystallisation occur in mafic (52–54 wt.% SiO2) lavas at Tengchong volcanic field. These early formed zircons with high δ18O (6.6‰–7.9‰) indicates mantle enrichment by subducted supracrustal materials. ABSTRACT Late Pleistocene (< 0.2 Ma) mafic and evolved volcanic rocks occur in northern Tengchong Volcanic Field, SE ...
Lizhu Wang, Haibo Zou
wiley +1 more source
Mapping global kimberlite potential from reconstructions of mantle flow over the past billion years.
PLoS ONE, 2022 Kimberlites are the primary source of economic grade diamonds. Their geologically rapid eruptions preferentially occur near or through thick and ancient continental lithosphere.
Anton Grabreck +2 more
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Geological Journal, EarlyView.Petrography, thermobarometry, and pseudosection modelling reveal peak metamorphic conditions of 3–7.5 kbar and 520°C–800°C in Tonian‐Cryogenian orthogneisses of the Dom Feliciano Belt. Metamorphic field gradients of 27°C/km–39°C/km and variable exhumation mechanisms support correlation of these units as remnants of a Himalayan‐type Piratini Orogeny ...
Thaiane Niederauer‐Santos +6 more
wiley +1 more source
Constraints on the Fate of Delaminated Lithosphere in the Upper and Mid‐Mantle
Geophysical Research LettersDelamination of lower continental lithosphere is known to have occurred under different tectonic settings. However, its fate in the mantle is poorly understood.
Ya‐Nan Shi, Jason P. Morgan
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Geochemistry, Geophysics, Geosystems, 2018 Assessing water contents of subduction zone mantle peridotites can gain insight into the compositions of slab‐derived fluids/melts and the active margin water cycle.
McKensie L. Kilgore +3 more
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Distribution and Processing of Highly Siderophile Elements in Cratonic Mantle Lithosphere
, 2016 Cratonic lithospheric mantle is composed of predominantly refractory materials that formed at higher mantle potential temperatures ( T P) than recorded in non-cratonic peridotites.
S. Aulbach, J. Mungall, D. G. Pearson
semanticscholar +1 more source