In this study, data from garnet-kyanite metapelites in ultrahigh-pressure (UHP) domains of the Western Gneiss Region (WGR), Norway, are presented. U–Pb geochronology and trace element compositions zircon, monazite, apatite, rutile garnet were acquired, pressure–temperature (P–T) conditions calculated using mineral equilibria forward modelling Zr-in-rutile thermometry. Garnet-kyanite gneiss Ulst...

Les condylomes correspondent à des verrues ano-génitales secondaires à une infection par Human Papilloma Virus (HPV). On distingue 3 formes cliniques qui peuvent être associées: les condylomes acuminés, papuleux et plans. Les condylomes acuminés sont les classiques crêtes de coq, tumeurs exophytiques à surface verruqueuse et hyperkératosique de couleur érythémateuse, grisâtre, ou chaire. Les co...

The Barrovian metamorphism of the Lepontine dome is manifested by isograds that cross-cut tectonic nappe contacts, which commonly interpreted as occurred after emplacement. However, pervasive mineral and stretching lineation in amphibolite facies, associated with top-to-foreland shearing, suggests peak conditions are coeval nappe-overthrusting. Here, we combine mapping U-Pb zircon dating to bet...

Rifted margins are often associated with widespread and thick evaporite (salt) deposits pronounced salt tectonics. The largest basins form during the latest stages of rifting, immediately prior to continental breakup. Salt tectonics along these commonly exhibit structural domains characterized by gravity-driven updip extension, translation, downdip shortening, nappe advance. precise spatial tem...