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1by Faccini, B., Bonadiman, C., Coltorti, M., Grégoire, M., Siena, F.“...], unusual for mantle wedge settings. Heavy rare earth elements and Al 2 O 3 and MgO contents in pyroxenes...”
Published in Journal of Petrology (2013)
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2by FACCINI, Barbara, BONADIMAN, Costanza, COLTORTI, Massimo, SIENA, Franca, Grègoire M.“... for mantle wedge settings. Heavy rare earth elements and Al2O3 and MgO contents in pyroxenes indicate a...”
Published in Journal of Petrology (2013)
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3by FACCINI, Barbara, BONADIMAN, Costanza, COLTORTI, Massimo, SIENA, Franca, Grègoire M.“... for mantle wedge settings. Heavy rare earth elements and Al2O3 and MgO contents in pyroxenes indicate a...”
Published in Journal of Petrology (2013)
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4“... Nd and 206 206Pb/ 204 Pb) that is due to increasing metasomatic enrichment of the mantle wedge via...”
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5by Ramírez de Arellano, Cristóbal, Calderón, Mauricio, Rivera, Huber, Valenzuela, Mauricio, Fanning, C. Mark, Paredes, Eliot“... and are typical products of continental magmatic arcs, where focused metasomatism of the mantle wedge results...”
Published in Journal of South American Earth Sciences (2021)
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6by NUCCIO, Pasquale, STUART FM, DI LIBERTO V, ELLAM RM“...Pb/204Pb) that is due to increasing metasomatic enrichment of the mantle wedge via subduction...”
Published in Geochemistry, Geophysics, Geosystems (2008)
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7“... metasomatic enrichment of the mantle wedge via subduction of the Ionian Adriatic plate since 30 Ma...”
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8“... contamination of slab window melts with arc components ‘stored’ in the supraslab mantle wedge and/or basal...”
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9by Gutiérrez, F., Gioncada, A., González Ferrán, O., Lahsen Azar, Alfredo, Mazzuoli, R.“... partial melting processes, while the mantle wedge is deeply modified by subduction-related components...”
Published 2005
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10“... window melts with arc components 'stored' in the supraslab mantle wedge and/or basal continental...”
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11by Bindeman, I. N., Eiler, J. M., Yogodzinski, G. M., Tatsumi, Y., Stern, C. R., Grove, T. L., Portnyagin, Maxim, Hoernle, Kaj, Danyushevsky, L. V.“... isotopic exchange with the mantle wedge before eruption. Finally, ......”
Published in Earth and Planetary Science Letters (2005)
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12by Bindeman, IN, Eiler, JM, Yogodzinski, GM, Tatsumi, Y, Stern, CR, Grove, TL, Portnyagin, M, Hoernle, K, Danyushevsky, LV“... isotopic exchange with the mantle wedge before eruption. Finally, adakites might not be slab melts at all...”
Published in Earth and Planetary Science Letters (2005)
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13by Bindeman, IN, Eiler, JM, Yogodzinski, GM, Tatsumi, Y, Stern, CR, Grove, TL, Portnyagin, MV, Hoemle, K, Danyushevsky, LV“... with the mantle wedge before eruption. Finally, adakites might not be slab melts at all, and instead come from...”
Published in Earth and Planetary Science Letters (2005)
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14by Bindeman, I. N., Eiler, J. M., Yogodzinski, G. M., Tatsumi, Y., Stern, C. R., Grove, T. L., Portnyagin, M., Hoernle, K., Danyushevsky, L. V.“... generated with more extreme δ^(18)O values, but undergo isotopic exchange with the mantle wedge before...”
Published in Earth and Planetary Science Letters (2005)
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15by Martelli, M., Nuccio, P. M., Stuart, F., Di Liberto, V., Ellam, R.“...) that is due to increasing metasomatic enrichment of the mantle wedge via subduction of the Ionian-Adriatic...”
Published in Geophysical Research Letters (2007)
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16by Martelli, M., Nuccio, P. M., Stuart, F., Di Liberto, V., Ellam, R.“...) that is due to increasing metasomatic enrichment of the mantle wedge via subduction of the Ionian-Adriatic...”
Published in Geochemistry, Geophysics, Geosystems (2008)
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