Fluid-inclusion studies of high-grade metamorphic rocks of the Ashuanipi complex, eastern Superior Province: constraints on the retrograde P-T path and implications for gold metallogeny

In this paper, we prove regularity properties of the boundary of the optimal shapes Ω ∗ in any case and in any dimension.. Full regularity is obtained in

If d = 2, in order to have the regularity of the whole boundary, we have to show that Theorem 6.6 and Corollary 6.7 in [1] (which are for solutions and not weak-solutions) are

Accordingly, a binding assay using GST-tagged recombinant Nup107 proteins and in vitro transcribed and translated full length Nup133 showed that a C-terminal truncation mutant

In this paper, we prove regularity properties of the boundary of the optimal shapes Ω ∗ in any case and in any dimension.. Full regularity is obtained in

The time- calibration of the pressure±temperature path is based on U±Pb dating of single zircon and monazite grains and titanite separates, on 40 Ar/ 39 Ar ages obtained by

Mineral abbreviations after Kretz (1983): Cld, chloritoid; Ttn, titanite; Grt, garnet; Czo, clinozoisite (incl. epidote); Lws, lawsonite; Tur, tourmaline; Cpx, clinopyroxene

Abstract Four metasedimentary zircon populations from different tectonometamorphic units of the Central and the Northern Schwarzwald (Variscan belt, SW- Germany) were investigated

40 Ar/ 39 Ar crystallization ages (between 20 and 15 Ma) appears related to brittle-ductile normal faulting and likely associated with the onset of Aegean back-arc