Published August 16, 2025 | Version v1
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Pistone M., Toy V.G., M.W. Ofman, Formo E., Robyr M. (2025) Supplementary materials associated to the peer-reviewed contribution on "Can pseudotachylytes form via fracture-induced decompression melting under hydrous conditions?", published in Tektonika

Authors/Creators

  • 1. ROR icon University of Georgia
  • 2. ROR icon Johannes Gutenberg University Mainz
  • 3. ROR icon University of Otago
  • 4. EDMO icon The University of Georgia
  • 5. ROR icon University of Lausanne

Description

These supplementary materials contain details about the the analytical investigations and thermodynamic modelling along with data and images acquired through different analytical instruments. Presentation of the methods, results, and discussion upon data are detailed in the work by Pistone M, Toy V.G., M.W. Ofman, Formo E., Robyr M. (2025) Can pseudotachylytes form via fracture-induced decompression melting under hydrous conditions? published in Tektonika. Here is the official citation as published in Tektonika:

Pistone, M., Toy, V., Ofman, M., Formo, E., & Robyr, M. (2025). Can Pseudotachylytes Form via Fracture-Induced Decompression Melting Under Hydrous Conditions?. τeκτoniκa, 3(2), 58–80. https://doi.org/10.55575/tektonika2025.3.2.64

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Pistone_Tektonika_Supplementary Materials.pdf

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Additional details

Funding

Swiss National Science Foundation
2016 Petrophysics of the Melt Connectivity Transition: Petrological, Rheological, and Seismic Characterisation of the Continental Moho PZ00P2_168166

Dates

Available
2025-08-15

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