reactions during deformation at lower crustal conditions: phase equilibrium modelling and U – Pb dating of zircon, monazite, rutile and titanite from the Kalak Nappe Complex, northern Norway

The age of int rusion of the trond hjem ite body at the type lo- cality at F oll stad is esti mated at 432 ± 3 Ma from overlap ping concordant zircon and titanite U-Pb analyses

A dolerite dyke cutt ing very low-grade metasedim entary rocks of the Lekvi kfjellet Group near Hamning berg, NE Varange r Peninsula, Finnmark, has yielded a U-Pb zircon upper

Zircons extracted from a felsic sheet in the bimodal, magmatic, Fånes complex of the Støren Nappe on Frosta peninsula yielded a U–Pb age of 488 ± 5 Ma, interpreted as the age

Taken in conjunctio n with isotopic data reported earlier, the zircon age for the Mok levatnet pluto n indica- tes that the magmatic activity represented in the Gjersvik Nappe extend

An elongate tonalite pluton and a c.10 m-thick granodiorite body in the southeastern part of the Bindal Batholith and Helgeland Nappe Complex, Nord-Trøndelag, have yielded U-Pb

One pelite sample from the contact aureole to the Egersund anorthosite complex in the Sveconorwegian province, Rogaland contains monazite inclusions in garnet that yield a mean age

The most developed model accounted for the delayed superimposed slow component of oxygen uptake and the influence of lactic power production on the oxygen kinetics.. The rate of

The model for electromagnetic interference due to radiation from the wind turbines basically extrapolates the electrical field strength from the distance at which the measurement