Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …

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

A model that places development of IOCG (and porphyry-epithermal) mineralization at ca.
1.60–1.575 Ga in eastern Proterozoic Australia into the context of a modern-day …

The evolution of Earth's biosphere, atmosphere and hydrosphere is tied to the formation of
continental crust and its subsequent movements on tectonic plates. The supercontinent …

Both medium-and high-pressure pelitic granulites were found in the Jiaobei massif in the
southern segment of the Jiao-Liao-Ji Belt, which is a Paleoproterozoic tectonic belt in the …

The Central Indian Tectonic Zone, because of its critical position in the tectonic framework of
East Gondwanaland, holds insights into our understanding of the assembly and dispersal of …

The Australian continent records c. 1860–1800 Ma orogenesis associated with rapid
accretion of several ribbon micro-continents along the southern and eastern margins of the …

Abstract From the Mesoproterozoic to Cambrian, Australo-Antarctica was characterised by
tectonic reconfiguration as part of the supercontinents Columbia, Rodinia and Gondwana …

Studies of pelitic gneisses and schists within the Yenisey regional shear zone (Garevka
complex) at the western margin of the Siberian craton provide important constraints on the …

The growth and dissolution behaviour of detrital, metamorphic and magmatic monazite and
zircon during granulite-facies anatexis in pelitic and psammo-pelitic granulites and in …