Evolution of shear zones through the brittle-ductile transition: The Calamita Schists (Elba Island, Italy)

Samuele Papeschi, Giovanni Musumeci, Francesco Mazzarini

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DOI: 10.1016/j.jsg.2018.05.023
Published: 2018-08
Container: Journal of Structural Geology
Publisher: Elsevier BV
Open access: unknown

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Cite this work

BibTeX

@article{allodium:10.1016/j.jsg.2018.05.023,
  title = {Evolution of shear zones through the brittle-ductile transition: The Calamita Schists (Elba Island, Italy)},
  author = {Samuele Papeschi and Giovanni Musumeci and Francesco Mazzarini},
  year = {2018},
  journal = {Journal of Structural Geology},
  doi = {10.1016/j.jsg.2018.05.023},
  url = {https://doi.org/10.1016/j.jsg.2018.05.023}
}

RIS

TY  - JOUR
TI  - Evolution of shear zones through the brittle-ductile transition: The Calamita Schists (Elba Island, Italy)
AU  - Samuele Papeschi
AU  - Giovanni Musumeci
AU  - Francesco Mazzarini
PY  - 2018
JO  - Journal of Structural Geology
DO  - 10.1016/j.jsg.2018.05.023
UR  - https://doi.org/10.1016/j.jsg.2018.05.023
ER  -

APA

Papeschi, S., Musumeci, G., & Mazzarini, F. (2018). Evolution of shear zones through the brittle-ductile transition: The Calamita Schists (Elba Island, Italy). Journal of Structural Geology. https://doi.org/10.1016/j.jsg.2018.05.023

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crossref · retrieved 2026-11-03T18:27:46.016Z