U-Pb age of the 2016 Amatrice earthquake causative fault (Mt. Gorzano, Italy) and paleo-fluid circulation during seismic cycles inferred from inter- and co-seismic calcite

Autor: Curzi M.[1, Bernasconi S.M.[3], Billi A.[4], Boschi C.[5], Aldega L.[1], Franchini S.[1], Albert R.[7], Gerdes A.[7], Barberio M.D.[1], Looser N.[3], Carminati E.[1]

Publikováno v: Tectonophysics (Amst. Online) 819 (2021): 1–18. doi:10.1016/j.tecto.2021.229076
info:cnr-pdr/source/autori:Curzi M.[1,2], Bernasconi S.M.[3], Billi A.[4], Boschi C.[5], Aldega L.[1], Franchini S.[1], Albert R.[7], Gerdes A.[7], Barberio M.D.[1], Looser N.[3], Carminati E.[1]/titolo:U-Pb age of the 2016 Amatrice earthquake causative fault (Mt. Gorzano, Italy) and paleo-fluid circulation during seismic cycles inferred from inter-and co-seismic calcite/doi:10.1016%2Fj.tecto.2021.229076/rivista:Tectonophysics (Amst. Online)/anno:2021/pagina_da:1/pagina_a:18/intervallo_pagine:1–18/volume:819

The Mt. Gorzano Fault (MGF) is a major seismically active extensional fault of the central Apennines, responsible for the destructive Mw 6.0 Amatrice earthquake in 2016. The MGF developed during post-orogenic extensional tectonics, generating a conti

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https://doi.org/10.1016/j.tecto.2021.229076