Ocean crust accretion along a high-temperature detachment fault in the Oman ophiolite: A structural and petrological study of the Bahla massif-Reference-Cited by-同舟云学术

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

Published:2022-01 Issue: Volume:822 Page:229160
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

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

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference105 articles.

1. Caractéristiques pétrographique, géochimique et structural de la section crustale profonde de l'ophiolite d'Oman : implications pour la genèse des magmas et le fonctionnement des chambres magmatiques à l'aplomb d'un centre d'expansion océanique;Abily,2011

2. The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-MgO melts, or both?;Abily;Geology,2013

3. Syn-magmatic normal faulting in the lower oceanic crust: evidence from the Oman ophiolite;Abily;Geology,2011

4. Geology and petrology of the plutonic complexes in the wadi Fizh area: multiple magmatic events and segment structure in the northern Oman ophiolite;Adachi;Geochem. Geophys. Geosyst.,2003

5. Plate acceleration : the obduction trigger ?;Agard;Earth Planet. Sci. Lett.,2007

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