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scopus(16)
(Interpretation of the Sanaga fault zone through remote sensing ( Cameroon). Its location within the big fault zones of Central Africa and of the northern boundary of the Congolese craton).
ArticleAbstract: Observation of lines and curved structures on the Landsat image no 199-57 has been interpreted as aPalabras claves:Autores:Jean François DumontFuentes:scopus(Observations on Landsat images of alignments in the Antalya travertines: discussion of the probable relations between neotectonic activity and hydrogeology).
ArticleAbstract: An Additive Color Viewer was used on Landsat images of 14 September 1975 for an alignment study of tPalabras claves:Autores:Aydar C., Jean François DumontFuentes:scopus(The importance of alternate compressive and extensional tectonic phases in the evolution of intracontinental faults in south-west Turkey).
ArticleAbstract: Neotectonic field analysis of Neogene and Quaternary fault mechanisms in Southwestern Anatolia enablPalabras claves:Autores:Jean François Dumont, Letouzey J., Uysal S.Fuentes:scopusAnalyses of fault mechanisms and expansion of southwestern Anatolia since the late Miocene
ArticleAbstract: Neotectonic field studies and detailed analyses of Neogene and Quaternary fault mechanisms in southwPalabras claves:Autores:Angelier J., Jean François Dumont, Karamanderesi H., Poisson A., Şimşek S., Uysal S.Fuentes:scopusActive subsidence controlled by basement structures in the Maranon Basin of northeastern Peru
Conference ObjectAbstract: The Maranon Basin is located between the Brazilian shield and the Andean foothills. The southern parPalabras claves:Autores:Garcia F., Jean François DumontFuentes:scopusFormation of the grabens in southwestern Anatolia.
ArticleAbstract: Tectonic compression and tensional directions at the Miocene-Quaternary interval are determined on tPalabras claves:Autores:Jean François Dumont, Karamanderesi I., Letouzey J., Şimşek S., Uysal S.Fuentes:scopusGeological constraints on the kinematics and fault-plane solution of the Quiches Fault Zone reactivated during the 10 November 1946 Ancash earthquake, northern Peru
ArticleAbstract: The earthquake (Mw=6.8) produced surface faulting along the Quiches normal-slip fault. Field studiesPalabras claves:Autores:Bellier O., Jean François Dumont, Mercier J.L., Sébrier M.Fuentes:scopusFluvial shifting in the Ucamara Depression as related to the neotectonics of the Andean foreland Brazilian craton border (Peru)
ArticleAbstract: Active and abandoned fluvial landforms observed on the present day surface of the Ucamara DepressionPalabras claves:Autores:Jean François DumontFuentes:scopusMorphologic evidence of active motion of the Zambapala Fault, Gulf of Guayaquil (Ecuador)
ArticleAbstract: The Zambapala Fault Zone (ZFZ) is located at the link between the offshore structures of the Gulf ofPalabras claves:Active strike-slip fault, Coastal morphology, Deflected stream channel, ECUADOR, Holocene, tectonic geomorphologyAutores:Essy Santana, Jean François Dumont, Vilema W.Fuentes:scopusMorphostructural provinces and neotectonics in the Amazonian lowlands of Peru
ArticleAbstract: The Amazonian lowlands of Peru are composed of the Subandean Zone (foreland), the Marañón Basin (forPalabras claves:Autores:Deza E., Garcia F., Jean François DumontFuentes:scopus