Fluid-rock interaction related to alpine subduction of Allalingabbro deduced from large-size μXRF element maps
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Publisher
Elsevier BV
Reference53 articles.
1. Initial Water Budget: The Key to Detaching Large Volumes of Eclogitized Oceanic Crust Alongthe Subduction Channel? Lithos (2010);Angiboust,2010
2. Permeability of subducted oceanic crust revealed by eclogite-facies vugs;Angiboust;Geology,2022
3. The Zermatt-Saas ophiolite: the largest (60-km wide) and deepest (c. 70–80 km) continuous slice of oceanic lithosphere detached from a subduction zone?;Angiboust;Terra Nova,2009
4. Channelized fluid flow and eclogite-facies metasomatism along the subduction shear zone;Angiboust;J. Petrol.,2014
5. The gabbro-eclogite transformation: an oxygen isotope and petrographic study of west Alpine ophiolites;Barnicoat;J. Metamorph. Geol.,1997
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