The Northern Apennines hinterland has been interpreted as a back-arc where magma emplaced in an active tectonic setting. However, the lack of constraints on the depth and setting of magma emplacement has led to contrasting tectonic, emplacement, and exhumation models. As part of project MIGRATE, funded by the SNFS, we (1) provide the first depth constraints on the Zuccale Fault and (2) document the emplacement of the Campiglia Marittima plutons in a contractional setting.
Geologic and metamorphic constraints on magma emplacement to validate regional seismic tomography of Tuscany (Project MIGRATE)
Papeschi Samuele
Primo
Writing – Original Draft Preparation
;Bonini MarcoSecondo
Membro del Collaboration Group
;Lanari RiccardoMembro del Collaboration Group
;Montanari DomenicoPenultimo
Funding Acquisition
;Del Ventisette ChiaraUltimo
Funding Acquisition
2024
Abstract
The Northern Apennines hinterland has been interpreted as a back-arc where magma emplaced in an active tectonic setting. However, the lack of constraints on the depth and setting of magma emplacement has led to contrasting tectonic, emplacement, and exhumation models. As part of project MIGRATE, funded by the SNFS, we (1) provide the first depth constraints on the Zuccale Fault and (2) document the emplacement of the Campiglia Marittima plutons in a contractional setting.File in questo prodotto:
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DRT-2024-Papeschi MIGRATE.pdf
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Descrizione: Geologic and metamorphic constraints on magma emplacement to validate regional seismic tomography of Tuscany (Project MIGRATE)
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