Metamorphic controls on seismic velocity of subducted oceanic crust at 100-250 km depth

Details Metamorphic controls on seismic velocity of subducted oceanic crust at 100-250 km depth Metamorphic controls on seismic velocity of subducted oceanic crust at 100-250 km depth

Nov 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002e%26psl.204...61c&link_type=abstract

Earth and Planetary Science Letters, Volume 204, Issue 1-2, p. 61-74.

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Scientific paper

Most circum-Pacific subduction zones at 100-250 km depth contain layers in which seismic velocities are ca. 5% slower than in the adjacent mantle. We compute seismic velocities from thermodynamic data for equilibrium metabasalt mineralogies, determined by free energy minimization, at subduction zone conditions. Lawsonite stability has a profound effect on seismic velocities of subducted oceanic metabasalts. Velocity reductions of 3-7% are estimated for lawsonite-eclogites derived by metamorphism of hydrothermally altered oceanic basalt subducted along relatively cool geotherms, whereas a 2-4% velocity increase is characteristic of anhydrous eclogites within the coesite stability field. The restricted depth extent of low-velocity layers is explicable through the influence of the coesite-stishovite transition, which reduces lawsonite stability at high pressure. This transition also increases the positive velocity anomaly in anhydrous eclogites to 4-6%, an effect that may account for deep high-velocity layers. The quality of the match between the properties of lawsonite-eclogite and low-velocity layers supports the contention that significant quantities of volatiles are retained within the oceanic crust beyond sub-arc depths. Because the velocity anomalies are explicable in terms of equilibrium phase relations, we find no reason to invoke metastability of metamorphic reactions to explain the low-velocity layers.

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