Abstract The rates and mechanisms by which deeply subducted continental crust was exhumed back to the surface are not well understood, but can be better characterized using multimineral petrochronology. Here, we combine zircon, titanite, apatite U-Pb ages from leucogranite phengite gneiss with a pressure–temperature (P–T) path eclogite provide robust quantitative constraints on cooling exhumati...

Artificial electrostatic potentials can be present in supercells constructed for atomistic simulations of surfaces and interfaces ionic crystals. Treating the ions as point charges, we systematically derive an formalism model systems increasing complexity, both neutral charged, with either open or periodic boundary conditions. This allows to correctly interpret results classical which are direc...

The high-pressure (HP) eclogites in the central Himalaya provide insights into metamorphism and exhumation history of crustal material beneath Tibetan plateau. Due to paucity exposure, nature timing protolith remain poorly known. Here we report zircon titanite U–Pb ages, bulk-rock mineral compositions Hf isotope data on from Thongmön Kharta areas Himalaya. record peak HP eclogite-facies at >1.6...