Constraints on Bend‐Faulting and Mantle Hydration at the Marianas Trench From Seismic Anisotropy

Abstract Subduction zones are a key link between the surface water cycle and the solid Earth, as the incoming plate carries pore water and hydrous minerals into the subsurface. However, water fluxes from surface to subsurface reservoirs over geologic time are highly uncertain because the volume of w...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:	Geophysical Research Letters
المؤلفون الرئيسيون:	Hannah F. Mark, Daniel Lizarralde, Douglas A. Wiens
التنسيق:	مقال
اللغة:	الإنجليزية
منشور في:	Wiley 2023-05-01
الموضوعات:	anisotropy serpentinization solid‐Earth water cycle subduction Marianas Trench
الوصول للمادة أونلاين:	https://doi.org/10.1029/2023GL103331

مواد مشابهة

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