Earth is the only planet known to be habitable, and is also unique with its liquid water, and
the operation of plate tectonics. The geological record shows that the habitability of our …

Abstract Although Jaillard's (2022) paper denotes the first attempt to propose a model for the
orogeny build-up of the Ecuadorian Andes, it is based on endorsing the poorly constrained …

Abstract The Darongshan-Shiwandashan granite belt (DSGB) is composed of S-type
granites and granodiorite intrusions, which are characterized by high-or ultrahigh …

The timing and mechanism of ultrahigh-temperature (UHT) granulite facies metamorphism is
critical to understanding the tectono-thermal evolution of granulite terranes and their …

High-pressure (HP) and ultrahigh-temperature (UHT) granulites with a high geothermal
gradient (greater than 500° C/GPa) are prominent features of Paleoproterozoic orogenic …

Ultrahigh-temperature metamorphism (UHTM) is important for the evolution and long-term
stability of continental crust. The Anosyen domain in southeastern Madagascar is a well …

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

Abstract The Himalayan-Tibetan orogen experienced extensive thermal disturbance during
the Indian-Asian collision, yet evidence for ultrahigh-temperature metamorphism (UHTM,> …

The crustal evolution of the southernmost∼ 2000–1800 Ma Trans‐Hudson orogen (THO) is
enigmatic due to burial by Phanerozoic sediments. We provide new insights through …

It remains unresolved whether extensive granitoids can originate from ultrahigh‐temperature
crustal anatexis beyond the stability of fusible hydrous minerals and, if any, how they are …