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Beneath the Western Alps, seismic tomography reveals a subduction graveyard at 500-600 km depth.

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Thermodynamic modeling of the replacement process shows that hydrous assemblages (involving phengite and allanite) formed at these stages.

Subunits within Sesia show a somewhat different conditions, the range being 1.6 – 1.9 GPa, 600 - 650 °C.

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, (1)Department of Geological Sciences, University of Bern, Baltzerstrasse 1, Bern, CH3012, Switzerland, (2)School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth, PL4 8AA, United Kingdom, [email protected], regardless of their composition, show essentially brittle behavior during subduction, down to 100 km or more.

However, tectonic strain may induce fractures and enhance permeability to fluids, thus promoting reequilibration, with dramatic effects on rock properties. The Sesia Zone (Western Alps) is best known for its spectacular eclogites, but the dominant rocks resulting from Cretaceous subduction of continental basement are metasediments, notably eclogitic micaschists.

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