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CONFERENCE
Une conférence de trois heures qui s’inscrit dans le Thème
«PHOSPHATOGENESE TERTIAIRE : EVIDENCES DE LA SOURCE MAGMATIQUE
DES ELEMENTS ET LITHOFACIES ASSOCIES», sera donnée par Monsieur Saïd
TLIG, Professeur au Département de Géologie, à la Faculté des Sciences de
Tunis (Université Tunis-El Manar)
Le Jeudi 30 mai 2013 à l’Amphi BG
A partir de 10 heures
Echarde de verre à microlites, et lapillis Lapilli à porphyroblastes de feldspaths
Cette conférence qui est destinée à contribuer au renforcement des capacités des
Doctorants et des Cadres, peut intéresser des Chercheurs et des Ingénieurs de
différentes spécialités (Géologie, Chimie, Biologie). Ses mots clés sont comme
suit : révocation des nappes ; précisions sur les faciès de l’Eocène et sur la
géodynamique des bassins tellien et sillon Tunisien ; magmatisme
éocène source des éléments nutritifs (nature et composition) ; et les
upwellings ?!; place des fossés dans la paléogéographie de l’Eocène ;
tectonique éocène et bassins anoxiques ; modélisation géochimique : Océan
Mondial sous-saturé en Si, P, … et rôle de la Pompe Biologique ; Corollaire
de Krauskopf (1953) ; gradients géochimiques indicateurs de source des
éléments (nutritifs et traces : REE ; LILE, HFSE, transitions 3d); procédés de
transformation (H2SO4 ; HCl) ; phosphogypse et environnement ; évaluation
de la radioactvité.
Vous y êtes cordialement invités.

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  • 1. CONFERENCE Une conférence de trois heures qui s’inscrit dans le Thème «PHOSPHATOGENESE TERTIAIRE : EVIDENCES DE LA SOURCE MAGMATIQUE DES ELEMENTS ET LITHOFACIES ASSOCIES», sera donnée par Monsieur Saïd TLIG, Professeur au Département de Géologie, à la Faculté des Sciences de Tunis (Université Tunis-El Manar) Le Jeudi 30 mai 2013 à l’Amphi BG A partir de 10 heures Echarde de verre à microlites, et lapillis Lapilli à porphyroblastes de feldspaths Cette conférence qui est destinée à contribuer au renforcement des capacités des Doctorants et des Cadres, peut intéresser des Chercheurs et des Ingénieurs de différentes spécialités (Géologie, Chimie, Biologie). Ses mots clés sont comme suit : révocation des nappes ; précisions sur les faciès de l’Eocène et sur la géodynamique des bassins tellien et sillon Tunisien ; magmatisme éocène source des éléments nutritifs (nature et composition) ; et les upwellings ?!; place des fossés dans la paléogéographie de l’Eocène ; tectonique éocène et bassins anoxiques ; modélisation géochimique : Océan Mondial sous-saturé en Si, P, … et rôle de la Pompe Biologique ; Corollaire de Krauskopf (1953) ; gradients géochimiques indicateurs de source des éléments (nutritifs et traces : REE ; LILE, HFSE, transitions 3d); procédés de transformation (H2SO4 ; HCl) ; phosphogypse et environnement ; évaluation de la radioactvité. Vous y êtes cordialement invités.