Paul Broquet

Caracteres structuraux et dynamiques d'un bassin en transtension; la plate-forme tunisienne a l'Ypresien terminal

In Tunisia, Ypresian carbonate deposits occur on a platform preserving vestige of an inherited fault network. The fault network delineates blocks of different sizes accounting for the platform morphology and in turn for variation in thickness of the Ypresian sequence. The nummulitic limestone carapace of the Ypresian sequence is fractured by faults and joints of various orientations which are systematically sealed by marly beds of early Lutetian age. This indicates that the fault network was reactivated during late Ypresian. Geometric and kinematic study indicates that this strike slip late reactivation is accomodated by normal fault. These structures originated in soft sediment undergoing diagenesis. Depending on bed competency, both ductile and brittle deformation features were recognized in the fault. This superficial tectonic event represents, a recent reactivation of ancient fractures cartographically located on the boundaries of late Ypresian megablocks. Kinematic study of the deformation within and along the boundaries of one of these blocks, (Ousseltia block), indicates a late Ypresian, early Lutetian strike-slip distensive faulting dynamic. Stress-field orientation indicates a rapid re-orientation in time from a predominantly NW-SE extensional tectonic to a NE-SW extensional event. Stratigraphic dating of that tectonical crisis coincides with a turbulent period of relative motions between Europe and Africa.

Dépollution par méthode électrocinétique d'un matériau argileux dopé au cadmium. essai pilote

Abstract Electrokinetic treatment is a remediation technique for fine-grained soils. The feasibility and efficiency of transporting cadmium with this treatment are investigated at pilot scale in a 3.25 t clayey medium specimen spiked with cadmium nitrate solution and at an electrode spacing of 100 cm. Sulfuric acid is added to catholyte to neutralize the hydroxides generated at the cathode. A constant current density of 0.3 mA-cm−2 is applied. The test is conducted with cadmium at a concentration of 882 mg·kg−1 of dried matter. Cadmium was transported toward the catholyte and plated on the cathode. After 3 259 h of processing and an energy expenditure of 159 kWh·m−3, 98.5 % of the cadmium was removed.

Serie stratigraphique du Cozzo Cavolino (Madonies orientales, Sicile)

The Panormide limestone and dolomite series of the Madonies massif near Cozzo Cavolino (Sicily) consists of upper Jurassic gray to white, crystalline dolomites transgressively overlain by a thin scaglia of marls and schistose marly limestone. The transgressive bed is covered by a discontinuous conglomerate of limestone, gravel and dolomitic pseudo-oolitics. An Oligocene to Miocene flysch covers the conglomerate beds.