Ocean crust accretion along a high-temperature detachment fault in the Oman ophiolite: A structural and petrological study of the Bahla massif

Autor: Michel Grégoire, Mary-Alix Kaczmarek, Matthew Rioux, Mathieu Benoit, Marie Python, Mathieu Rospabé, Georges Ceuleneer, Bénédicte Abily

Publikováno v: Tectonophysics
Tectonophysics, Elsevier, In press, ⟨10.1016/j.tecto.2021.229160⟩
Tectonophysics (0040-1951) (Elsevier), 2022-01, Vol. 822, P. 229160 (18p.)
Tectonophysics, 2022, 822 (229160), pp.229160. ⟨10.1016/j.tecto.2021.229160⟩

International audience; The Bahla massif exposes the lower crustal section of the Oman ophiolite located close to the thrust front of the Semail nappe. It is affected by intense faulting previously attributed to tectonic events that dismembered a cla

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https://hal.archives-ouvertes.fr/hal-03456679