Articles | Volume 12, issue 6
Solid Earth, 12, 1357–1388, 2021
https://doi.org/10.5194/se-12-1357-2021
Solid Earth, 12, 1357–1388, 2021
https://doi.org/10.5194/se-12-1357-2021

Research article 16 Jun 2021

Research article | 16 Jun 2021

Interactions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoids

Laurent Jolivet et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on se-2021-11', Antonio Castro, 05 Mar 2021
    • AC3: 'Reply on RC1', Laurent Jolivet, 26 Apr 2021
  • CC1: 'Comment on se-2021-11_SP_GV_GM_FM', Samuele Papeschi, 29 Mar 2021
    • AC1: 'Reply on CC1', Laurent Jolivet, 29 Mar 2021
      • CC2: 'Reply on AC1', Samuele Papeschi, 31 Mar 2021
        • AC4: 'Reply on CC2', Laurent Jolivet, 26 Apr 2021
  • RC2: 'Comment on se-2021-11', Andrea Brogi, 30 Mar 2021
    • AC2: 'Reply on RC2', Laurent Jolivet, 30 Mar 2021
    • AC5: 'Reply on RC2', Laurent Jolivet, 26 Apr 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Laurent Jolivet on behalf of the Authors (27 Apr 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (29 Apr 2021) by Mark Allen
ED: Publish as is (30 Apr 2021) by Federico Rossetti(Executive Editor)
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Short summary
Although viscosity of the crust largely exceeds that of magmas, we show, based on the Aegean and Tyrrhenian Miocene syn-kinematic plutons, how the intrusion of granites in extensional contexts is controlled by crustal deformation, from magmatic stage to cold mylonites. We show that a simple numerical setup with partial melting in the lower crust in an extensional context leads to the formation of metamorphic core complexes and low-angle detachments reproducing the observed evolution of plutons.