Nature and distribution of slab‐derived fluids and mantle sources beneath the Southeast Mariana forearc rift

Subduction zone magmas are produced by melting depleted mantle metasomatized by fluids released from the subducted slab. In most subduction zones, formation of backarc basin (BAB) and arc magmas depletes the mantle source toward the trench, resulting in more depleted mantle beneath the forearc. Slab...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:Geochemistry, Geophysics, Geosystems
المؤلفون الرئيسيون: Julia M. Ribeiro, Robert J. Stern, Katherine A. Kelley, Fernando Martinez, Osamu Ishizuka, William I. Manton, Yasuhiko Ohara
التنسيق: مقال
اللغة:الإنجليزية
منشور في: Wiley 2013-10-01
الموضوعات:
Mariana arc
Mariana trough
subduction component
aqueous fluids
sediment melt
Southeast Mariana forearc rift
الوصول للمادة أونلاين:https://doi.org/10.1002/ggge.20244

الانترنت

https://doi.org/10.1002/ggge.20244

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