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                <term xml:lang="en">Armorican Massif</term>
                <term xml:lang="en">intraplate seismicity</term>
                <term xml:lang="en">Lorient earthquake</term>
                <term xml:lang="en">seismotectonics</term>
                <term xml:lang="en">stress tensor</term>
                <term xml:lang="fr">Surfaces continentales</term>
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              <p>Since it was one of the largest events ever recorded in this region, this was the opportunity to improve our seismotectonic knowledge of the Armorican Massif. We performed a post-seismic survey (SISBREIZH), which allowed us to locate accurately 62 aftershocks within 14 days. An analysis of the main shock using broadband records provided a normal fault mechanism with a dextral strike-slip component located at 12-km depth. The aftershock sequence exhibits: (1) a combination of almost pure right-lateral strike-slip and dominant normal faulting similar to the main shock; (2) magnitudes ranging from 0.4 to 1.9 and (3) depths ranging from 11.5 to 13.5 km, that is, close to the main shock hypocenter. The distribution of the aftershocks defines a rupture plane dipping 60 • to the south with a fault length of ≈2 km consistent with the source parameters of the main shock. Beside the SISBREIZH survey, a morpho-structural analysis has been conducted: we found fault plane solutions with southward-dipping N120-150 normal fault planes. The stress tensor computed after the aftershock focal mechanisms is a strike-slip regime with a NE-SW extensional direction. The Lorient earthquake appears to reactivate Late Hercynian structures and the whole sequence is reflecting the regional-scale tectonic stress field expressed by a combination of strike-slip and normal faulting.</p>
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