Syn?Orogenic Exhumation of High?P Units by Upward Extrusion in an Accretionary Wedge: Insights From the Eastern Elba Nappe Stack (Northern Apennines, Italy)

نویسندگان

چکیده

The E-vergent Northern Apennines formed by Oligocene-Miocene convergence and westward subduction of Adria beneath Europe. Extension ensued in the Mid-Late Miocene reflecting lower plate roll-back causing opening back-arc Tyrrhenian Sea. Post-orogenic extension is commonly advocated as main driver exhumation belt's inner domain high-pressure/low-temperature (HP-LT) rock units. Acquadolce Subunit Eastern Elba nappe stack contains HP-LT rocks recording peak blueschist conditions 1.5–1.8 GPa at 320°C–370°C loosely dated to Oligocene-Early Miocene. It sandwiched two Late Miocene, out-of-sequence top-to-the E thrusts between Jurassic LP serpentinites on top HT–LP contact metamorphosed marbles its base. We document widespread W-verging ductile asymmetries within Subunit, which correspond W extensional shearing for current orientation. This allowed early syn-orogenic from blueschist- greenschist-facies conditions, wherein coeval W-directed exhuming units acted synchronously with E-directed thrusting their base extrusion an overall contractional setting. basal, is, however, challenging wedge has since been reworked E-verging compressive tectonics, metamorphism, later extension, obliterating much evidence supporting during stages build-up. Syn-orogenic deep structural levels orogenic a viable mechanism account other exhumed part belt.

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ژورنال

عنوان ژورنال: Tectonics

سال: 2021

ISSN: ['0278-7407', '1944-9194']

DOI: https://doi.org/10.1029/2020tc006348