Ridge Subduction: Unraveling the Consequences Linked to a Slab Window Development Beneath South America at the Chile Triple Junction

نویسندگان

چکیده

Abstract The subduction of an active spreading center generates a clear signature in the temporal evolution zones. It disrupts typical arc‐type magmatism and intraplate seismicity, enhances emplacement backarc plateau lava profoundly change tectonics topographic relief. These distinct observations are commonly linked to slab window opening mantle upwelling. Chile Triple Junction provides ideal setup study mid‐ocean ridge process where both sides continue subduct. Here, we use 2‐D numerical petrological‐thermomechanical modeling focus on transient geodynamic processes caused by subduction. Model results show separation along axis with window. During opening, partial melts from migrate toward subcontinental high temperatures forearc predicted. modeled temperature is consistent observed heat flow data, high‐temperature metamorphism recorded Chilean rocks. Such migrated might explain low viscosity inferred seismic velocity anomalies imaged beneath South America, common geochemical Ridge, Taitao Ophiolite magmatism. Following separation, our models suggest uplift changes stress regime, which deformation records. Summarizing, model Ridge framework that explains diverse records magmatism, metamorphism, physical properties.

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ژورنال

عنوان ژورنال: Geochemistry Geophysics Geosystems

سال: 2023

ISSN: ['1525-2027']

DOI: https://doi.org/10.1029/2023gc010977