Thermal effects of variable material properties and metamorphic reactions in a three-component subducting slab

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Thermal Structure and Metamorphic Evolution of Subducting Slabs

Subducting lithospheric plates are the cool, downwelling limbs of mantle convection and the negative buoyancy of subducting slabs (slab pull) drives plate tectonics [Forsyth and Uyeda, 1975]. Subduction zones are regions of intense earthquake activity, explosive volcanism, and complex mass transfer between the crust, mantle, hydrosphere, and atmosphere. In this contribution, I present subductio...

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Dehydration of the subducting slab favors the melting of the surrounding mantle. Water content and melt evolution atop a spontaneously retreating subducting slab are reported in a threedimensional (3-D) model. We find that fluids, including water and melts in the rocks, vary substantially along the trench, which cannot be found in two-dimensional (2-D) models. Their maxima along the subducting ...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Solid Earth

سال: 2015

ISSN: 2169-9313

DOI: 10.1002/2015jb012080