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- W2006308870 abstract "New data on faults from the western-central area of the Corinth Gulf give new insights into the kinematics of this rift zone. The Xylokastro Fault was active 1 Myr ago and also around 108 ka. The Doumena Fault is younger than the Pirgaki Fault, so out-of-sequence, and was active 125 ka ago. Cements from two faults sampled on the northern coast have given two ages, respectively close to 300–400 ka and greater than 1 Myr. These new data confirm the recent fault activity on the two rift borders. To cite this article: C. Causse et al., C. R. Geoscience 336 (2004). De nouvelles datations sur les failles et fractures du centre-ouest du golfe de Corinthe permettent de préciser la cinématique de la zone. La faille de Xylokastro a enregistré des rejets il y a environ 1 Ma et autour de 108 ka. La faille de Doumena est postérieure à la faille de Pirgaki, donc out-of-sequence, et a joué il y a 125 ka. Les deux failles datées sur la côte nord ont respectivement des âges de l'ordre de 300–400 ka et supérieurs à 1 Ma. Ces données confirment l'activité sub-actuelle des failles sur les deux bordures du rift. Pour citer cet article : C. Causse et al., C. R. Geoscience 336 (2004)." @default.
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- W2006308870 date "2004-03-01" @default.
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- W2006308870 title "Kinematics of the Corinth Gulf inferred from calcite dating and syntectonic sedimentary characteristics" @default.
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- W2006308870 doi "https://doi.org/10.1016/j.crte.2003.11.017" @default.
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