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Title | The Dynamic Mass Transfer from Slabs to |
Description | Home Project Team Research Units Publications Communication Events Home Project Team Research Units Publications Communication Events The Dynamic Mass Tra |
Keywords | Bootstrap, Parallax, Template, Registration |
WebSite | prin2017dynastars.it |
Host IP | 89.46.109.28 |
Location | Italy |
Euro€281,371
Zuletzt aktualisiert: 2022-06-23 00:55:13
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Valore di acquisto/vendita | Euro€281,371 |
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Visitatori unici giornalieri | 2,165 |
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Home Project Team Research Units Publications Communication Events Home Project Team Research Units Publications Communication Events The Dynamic Mass Transfer from Slabs to Arcs Programma di Ricerca Scientifica di Rilevante Interesse Nazionale PRIN Project n. 2017ZE49E7 Formation of juvenile arc crust at ocean-continent convergent margins is a driving process for continental growth. It initiates with loss of COH-bearing fluids-melts from subducting oceanic plates, is driven by fluid-melt mediated mass transfer into supra-subduction the mantle wedge and causes mantle metasomatism and melting. Magma underplating beneath the arc crust enhances anatexis and differentiation of the continental crust. In this scenario, uncertainties still concern the evolution of fluid-melt/rock interaction with the sub-arc mantle and with the deep arc crust through temperature, space and time, and regard also the following challenging aspects: (a) the phase relations in slab and mantle wedge rocks in |
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