Volume diffusion of Pb occurs over micron length scales in apatite and rutile at temperatures
relevant to the evolution of the middle and lower crust. Continuous thermal history …

The study of magmatic and metamorphic processes is challenged by geological
complexities like geochemical variations, geochronological uncertainties and the …

Titanite U–Pb geochronology is a promising tool to date high-temperature tectonic
processes, but the extent to and mechanisms by which recrystallization resets titanite U–Pb …

Abstract The Dora‐Maira massif is an archetypal nappe stack of subducted and exhumed
upper crust. Slices of continental crust experienced metamorphism at upper blueschist to …

We combine monazite petrochronology with thermal modeling to evaluate the relative roles
of crustal melting, surface denudation, and tectonics in facilitating ultrafast exhumation of the …

Here, we study the relationships of titanite-hosting microdomains, intragrain chemical
variations, microstructure and fluids with the aim of deciphering the reliability of titanite U–Pb …

Variations of rare earth element (REE) concentrations in metamorphic garnet are an
important source of information of geodynamic and geochemical processes in the deeper …

Continued improvements in both ICPMS (inductively-coupled plasma mass spectrometry)
and laser ablation technologies are fueling advancements in accessory mineral …

Underexplored accessory minerals such as titanite and apatite have the potential to give
insights into the nature and the petrogenesis of their host rock. Their trace element and REE …

The trace element composition of titanite reflects the temperature, pressure and bulk‐rock
composition from which it crystallized. Two geochemical discriminators are identified by …