1995 (v1)
Publication
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Uploaded on: March 31, 2023
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Last name: PENNACCHIONI G.
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The cause of intermediate-depth (50-300 km) seismicity in subduction zones is uncertain. It is typically attributed either to rock embrittlement associated with fluid pressurization, or to thermal runaway instabilities. Here we document glassy pseudotachylyte fault rocks - the products of frictional melting during coseismic faulting - in the...