Imperial College London
Alternate

Saskia Goes

Faculty of Engineering, Department of Earth Science & Engineering

Professor of Geophysics
 
 
 
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Contact

 

+44 (0)20 7594 6434s.goes

 
 
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Location

 

4.47Royal School of MinesSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Perrin:2016:10.1002/2016GC006527,
author = {Perrin, A and Goes, S and Prytulak, J and Davies, DR and Wilson, C and Kramer, S},
doi = {10.1002/2016GC006527},
journal = {Geochemistry, Geophysics, Geosystems},
pages = {4105--4127},
title = {Reconciling mantle wedge thermal structure with arc lava thermobarometric determinations in oceanic subduction zones},
url = {http://dx.doi.org/10.1002/2016GC006527},
volume = {17},
year = {2016}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - Subduction zone mantle wedge temperatures impact plate interaction, melt generation, and chemical recycling. However, it has been challenging to reconcile geophysical and geochemical constraints on wedge thermal structure. Here we chemically determine the equilibration pressures and temperatures of primitive arc lavas from worldwide intraoceanic subduction zones and compare them to kinematically driven thermal wedge models. We find that equilibration pressures are typically located in the lithosphere, starting just below the Moho, and spanning a wide depth range of ∼25 km. Equilibration temperatures are high for these depths, averaging ∼1300°C. We test for correlations with subduction parameters and find that equilibration pressures correlate with upper plate age, indicating overriding lithosphere thickness plays a role in magma equilibration. We suggest that most, if not all, thermobarometric pressure and temperature conditions reflect magmatic reequilibration at a mechanical boundary, rather than reflecting the conditions of major melt generation. The magma reequilibration conditions are difficult to reconcile, to a first order, with any of the conditions predicted by our dynamic models, with the exception of subduction zones with very young, thin upper plates. For most zones, a mechanism for substantially thinning the overriding plate is required. Most likely thinning is localized below the arc, as kinematic thinning above the wedge corner would lead to a hot fore arc, incompatible with fore-arc surface heat flow and seismic properties. Localized subarc thermal erosion is consistent with seismic imaging and exhumed arc structures. Furthermore, such thermal erosion can serve as a weakness zone and affect subsequent plate evolution.
AU  - Perrin,A
AU  - Goes,S
AU  - Prytulak,J
AU  - Davies,DR
AU  - Wilson,C
AU  - Kramer,S
DO  - 10.1002/2016GC006527
EP  - 4127
PY  - 2016///
SN  - 1525-2027
SP  - 4105
TI  - Reconciling mantle wedge thermal structure with arc lava thermobarometric determinations in oceanic subduction zones
T2  - Geochemistry, Geophysics, Geosystems
UR  - http://dx.doi.org/10.1002/2016GC006527
UR  - http://hdl.handle.net/10044/1/40936
VL  - 17
ER  -
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