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    Upper-crust thermal evolution of the Patagonian Precordillera basement (Argentina): insights from fission track, (U-Th)/He thermochronology and geodynamic significance by Paulo Marcos (7459064)

    Published 2025
    “…This first stage might have resulted from coupled tectonothermal processes consisting of extensional faulting and high-temperature gradient. Subsequently, a relatively fast temperature decrease (2.75–5°C/My) for the late Early Cretaceous to Paleocene is likely related to a compressive stage associated with the growth of the early Andean Orogen. …”
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