Hydration of a Mantle Shear Zone Beyond Serpentine Stability: A Possible Link to Microseismicity Along Ultraslow Spreading Ridges?

Autor: J. F. Vieira Duarte, Othmar Müntener, Mary-Alix Kaczmarek, Benita Putlitz, Pierre Vonlanthen

Publikováno v: Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, 2020, 125, ⟨10.1029/2020JB019509⟩
Vieira Duarte, J. F.; Kaczmarek, M.-A.; Vonlanthen, P.; Putlitz, B.; Müntener, O. (2020). Hydration of a Mantle Shear Zone Beyond Serpentine Stability: A Possible Link to Microseismicity Along Ultraslow Spreading Ridges? Journal of Geophysical Research: Solid Earth, 125(10) American Geophysical Union 10.1029/2020JB019509
Journal of Geophysical Research: Solid Earth, vol. 125, pp. 1-24 (AN 019509)

International audience; Hydration of the oceanic mantle is a fundamental process of the global water cycle promoting chemical and volumetric changes and facilitating mantle exhumation along detachment faults. At which depth these processes occur and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e1ce2768f0c1282824638045531e0ef9
https://hal-insu.archives-ouvertes.fr/insu-03661435/document