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

Ultrahigh-temperature (UHT) metamorphic rocks associated with the 'Khondalite Belt'within
the Inner Mongolia Suture Zone (IMSZ) provide robust evidence for extreme thermal …

We report SHRIMP U–Pb zircon ages from two samples of Mg–Al granulite and one of
normal khondalite from the Khondalite belt of Inner Mongolia, North China Craton. These …

We report here for the first time the occurrence of Mg–Al granulites within the khondalite belt
of the North China Craton and provide robust evidence for extreme crustal metamorphism at …

A vast supracrustal belt of khondalites (granulite facies metapelites) occur along the
northern margin of the North China Craton. We report here for the first time spinel+ quartz …

Eight Re–Os ages from six molybdenite samples representative of the Cu–Mo–Au
mineralization at the giant Malanjkhand deposit in Madhya Pradesh were obtained using ID …

Regional metamorphic belts provide important constraints on the plate tectonic architecture
of orogens. We report here a detailed petrologic examination of the sapphirine-bearing ultra …

Rapid developments in the scope and quality of internally consistent thermodynamic data
sets arising from the incorporation of new experimental data and solid| solution models for …

The anhydrous mineral assemblages that characterize granulite facies rocks, including
charnockites and ultrahigh-temperature rocks, require that water activity was buffered to low …

The North China Craton (NCC) constitutes one of the fundamental Precambrian nuclei of
Asia. The Paleoproterozoic khondalite belt along the northern margin of the NCC shows …