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T. Bull, W. Pearthree, and P. , Frequency and size of Quaternary surface ruptures of the Pitaycachi fault, northeastern Sonora, Mexico. Bulletin of the Seismological Society of America, vol.78, issue.2, pp.956-978, 1988.

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. Le-graben-d-'acambay-est-un-bassin-intra-arc-majeur-de-la-ceinture-volcanique-trans-mexicaine-langridge, Trois systèmes de failles majeures définissent ce graben : la faille d'Acambay-Tismadejé localisée au niveau de la marge nord du graben, la faille Pastores formant la bordure sud et les failles intragraben (Figure 3, Les études de tranchées réalisées au niveau de 4 sites le long de la faille Acambay-Tixmadejé révèlent l'existence du séisme de 1912 (M b =6,9) et au moins 4 séismes datés du Pleistocène supérieur et de l'Holocène, 2000.

. Langridge, plusieurs cartes montrant les ruptures produites par le séisme d'Acambay sont réalisées (Figure 4, Basées sur les descriptions d'Urbina, 1913.

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. Le-séisme-d-'hebgen-lake-ayant-eu-lieu-en, est généré par un système complexe de failles normales, comprenant 2 segments (Hebgen Lake et Red Canyon), pour une longueur totale de 26 km. La faille de Red Canyon est caractérisée par une orientation SE-NO se transformant en orientation E-O, perpendiculaire à l'orientation de la faille d'Hebgen Lake. A partir de cette géométrie particulière, 1959.

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Z. Bernard, ainsi que la modélisation des données de nivellement (Arca et al., 1983) et les observations des ruptures à la surface permettent de définir la géométrie de ce système Il est composé de 2 structures de même orientation, mais de pendages différents (60° à l'ouest et 20° à l'est) La troisième structure ayant participé à la rupture est antithétique aux deux autres, avec un pendage de 70° vers le sud. A partir de la progression de la rupture, nous définissons les distances séparant ces différentes structures les unes des autres. Ainsi les deux failles de même orientation sont distantes d'environ 1,5 km, Les traces à la surface des failles responsables des 2 e et 3 e chocs, p.5, 1989.

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. Hubert, la partie est du rift de Corinthe a été marquée par l'occurrence de 3 séismes de magnitude ? 6 en moins d'une semaine Ces trois séismes montrent une progression vers l'est, EnJackson et al, 1981.

K. Alepohori, Les failles Pisia et Alepohori possèdent un pendage d'environ 60° vers le nord et sont distantes d'un kilomètre. La faille de Kaparelli possède un pendage de 60° vers le sud. Le mécanisme au foyer du premier séisme est localisé à une profondeur de 10km, tandis que les mécanismes des deux autres ont une profondeur de 8km. La distance entre les failles antithétiques Alepohori et Kaparelli est d'environ 10 km en prenant en compte les tracés à la surface de ces failles

. Hubert, Pisia qui n'ont pas rompu lors de ce séisme sont à des distances minimales de 3 km. L'existence de la faille offshore fait l'objet de plusieurs doutes, issues de l'observation de données géophysiques (communication personnelle SISCOR), la distance de la faille de Pisia avec la faille de Xylokastro plus à l'ouest est donc également prise en compte, Les failles les plus proches de la faille de De même les distances séparant la faille Kaparelli des failles situées plus au nord et à l'est sont intégrées dans l'étude, 1996.

. Hubert, Carte des épicentres des 3 séismes de 1981 accompagnée des principales failles de la zone, Figure, vol.12, 1996.

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A. Partir, observation de ce système et des incertitudes associées, nous considérons une distance séparant le segment de Willow Creek et Doublespring d'environ 1 km. Nous considérons une distance d'environ 5 km entre la faille de Doublespring participant à la génération de ce séisme et le

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. Le-séisme-d-'edgecumbe-en-nouvelle-zélande, Ml 6,3) est associé à la rupture tectonique de la faille d'Edgecumbe, des mouvemets sur les failles Onepu et Rotoitipakau et de nombreuses ruptures de surface sur les failles Awaiti, 1987.