Himalayan zircons resurface in Sumatran arc volcanoes through sediment recycling

نویسندگان

چکیده

Abstract Understanding the processes of subducted sediment recycling in subduction zones is vital to decipher Earth’s crust-mantle interactions. This study uses along-arc geochemical variations and zircon U-Pb-Hf-O isotopes Quaternary arc basalts andesites on Sumatra Island, Indonesia assess mode zones. The Hf-O inherited zircons near Toba Caldera indicate that some them were derived from terrigenous sediments mainly sourced (eastern) Himalaya. Hybridization with mantle also accounts for enriched Sr-Nd isotopic compositions volcanic rocks Caldera. Thermodynamic modeling indicates did not melt slab surface. Rather, evidence supports their formation as diapirs rise buoyantly through hot wedge contribute ~30 45% magma source Toba.

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ژورنال

عنوان ژورنال: Communications earth & environment

سال: 2022

ISSN: ['2662-4435']

DOI: https://doi.org/10.1038/s43247-022-00611-6