Dating the topography through thermochronology: application of Pecube code to inverted vertical profile in the eastern Sila Massif, southern Italy

Autor: Olivetti V.[1, Balestrieri M.L.[3], Faccenna C.[1], Stuart F.M.[4]

Publikováno v: Italian Journal of Geosciences
Italian Journal of Geosciences, 2017, 136 (3, SI), pp.321-336. ⟨10.3301/IJG.2016.09⟩
Italian Journal of Geosciences, Società Geologica Italiana, 2017, 136 (3, SI), pp.321-336. ⟨10.3301/IJG.2016.09⟩
Italian Journal of Geosciences (Testo stamp.) 136 (2017): 321–336. doi:10.3301/IJG.2016.09
info:cnr-pdr/source/autori:Olivetti V.[1,2], Balestrieri M.L.[3], Faccenna C.[1], Stuart F.M.[4]/titolo:Dating the topography through thermochronology: Application of Pecube code to inverted vertical profile in the eastern Sila Massif, southern Italy/doi:10.3301%2FIJG.2016.09/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2017/pagina_da:321/pagina_a:336/intervallo_pagine:321–336/volume:136

International audience; The Sila Massif is a small part of an orogenic wedge that sits on top of the narrow and active Calabrian subduction zone. The topography of the Sila Massif is characterized by a plateau region whose age and origin has been lon

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https://hal.science/hal-01765639