Biblioteca Digital

48 resultados para Subduction Rollback

em BORIS: Bern Open Repository and Information System - Berna - Suiça

Triassic asymmetric subduction rollback in the southern New England Orogen (eastern Australia): the end of the Hunter-Bowen orogeny

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Mantle wedge peridotites Fossil reservoirs of deep subduction zone processes Inferences from high and ultrahigh-pressure rocks from Bardane (Western Norway) and Ulten (Italian Alps)

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Yo-Yo subduction recorded by accessory minerals (Sesia Zone, Western Alps)

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Internal and External Fluid Sources for Eclogite-facies Veins in the Monviso Meta-ophiolite, Western Alps: Implications for fluid Flow in Subduction Zones

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Geochemistry of Ocean Floor and Fore-arc Serpentinites: Constraints on the Ultramafic Input to Subduction Zones

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The importance of talc and chlorite hybrid rocks for volatile recycling through subduction zones; evidence from the high-pressure subduction mélange of New Caledonia

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In Situ Laser-Ablation-ICP-MS chemical analysis of melt inclusion and prospects for constraining subduction zone magmatism

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High-pressure veins in eclogite from New Caledonia and their significance for fluid migration and seismic activity in subduction zones

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Aqueous fluids and hydrous melts in high-pressure and ultra-high pressure rocks: implications for element transfer in subduction zones

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Subduction-related metamorphism in the Alps: review of isotopic ages based on petrology and their geodynamic consequences

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From subduction to collision: Thermal overprint of HP/LT meta-sediments in the north-eastern Lepontine Dome (Swiss Alps) and consequences regarding the tectono-metamorphic evolution of the Alpine orogenic wedge

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Majoritic garnets monitor deep subduction fluid flow and mantle dynamics

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Subduction zone fluxes of halogens and noble gases in seafloor and forearc serpentinites

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Tethyan mantle metasomatism creates subduction geochemical signatures in non-arc Cu–Au–Te mineralizing magmas, Apuseni Mountains (Romania)

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Petrology and trace element budgets of high-pressure peridotites indicate subduction dehydration of pristine serpentinites (Cima di Gagnone, central Alps, Switzerland)

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