| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441062 | Lithos | 2011 | 17 Pages |
Abstract
⺠Several eclogite-facies shear zones across a coherent slice of oceanic lithosphere. ⺠Coexistence of brittle and plastic deformation within the lawsonite-eclogite facies. ⺠Dissemination of eclogite clasts along the Shear Zones. ⺠Locally pervasive fluid flow led to the crystallization of hydrated paragenesis.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
S. Angiboust, P. Agard, H. Raimbourg, P. Yamato, B. Huet,