Born in Lyon,France,in 1941,ProfessorJacques Charvet was a student at EcoleNormale Supérieure de Saint-Cloud(1961-1965)and at the same time studied geologyat Paris University.After the“agrégation”(acompeti...Born in Lyon,France,in 1941,ProfessorJacques Charvet was a student at EcoleNormale Supérieure de Saint-Cloud(1961-1965)and at the same time studied geologyat Paris University.After the“agrégation”(acompetitive examination),he began his careerat the University of Lille in 1965,where hewas initially appointed as lecturer.Besides his teaching duties,he startedfield research in former Yugoslavia(Bosnia-Herzegovina and Croatia),under the guidanceof Prof.Paul Celet,to obtain the old style(long term)French Doctor’s Degree.Hestudied the stratigraphy,paleogeography andstructural evolution of the Dinarides alongthe transect Mostar-Sarajevo-Tuzla.Thisstudy led to the reconstruction of ageodynamic evolutionary model,from theTriassic rifting of the African margin to thelast oceanic closure and collision withEurope,emphasizing the existence of a majorLate Jurassic tectonic event,underlined byophiolite obduction,before the Tertiary finalpiling of nappes.展开更多
文摘Born in Lyon,France,in 1941,ProfessorJacques Charvet was a student at EcoleNormale Supérieure de Saint-Cloud(1961-1965)and at the same time studied geologyat Paris University.After the“agrégation”(acompetitive examination),he began his careerat the University of Lille in 1965,where hewas initially appointed as lecturer.Besides his teaching duties,he startedfield research in former Yugoslavia(Bosnia-Herzegovina and Croatia),under the guidanceof Prof.Paul Celet,to obtain the old style(long term)French Doctor’s Degree.Hestudied the stratigraphy,paleogeography andstructural evolution of the Dinarides alongthe transect Mostar-Sarajevo-Tuzla.Thisstudy led to the reconstruction of ageodynamic evolutionary model,from theTriassic rifting of the African margin to thelast oceanic closure and collision withEurope,emphasizing the existence of a majorLate Jurassic tectonic event,underlined byophiolite obduction,before the Tertiary finalpiling of nappes.
