Ultrahigh-temperature (UHT) metamorphism is the most thermally extreme type of crustal
metamorphism, with the crust capable of withstanding temperatures≥ 900° C. Mineral …

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

In general, Archean rocks exhibit rather ordinary moderate-P-high-T facies series
metamorphism; neither blueschists nor any record of deep continental subduction and return …

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

The Precambrian geologic history of Peninsular India covers nearly 3.0 billion years of time.
India is presently attached to the Eurasian continent although it remains (for now) a separate …

Ultrahigh-temperature (UHT) crustal metamorphism is a division of medium-pressure
granulite facies metamorphism where peak temperatures of 900–1100° C have been …

The Eastern Ghats belt is a large high-grade terrane exposed along the east coast of India.
The late Proterozoic orogen consists of N–S trending charnockite and metasedimentary …

We present possible tectonic models for two crustal domains of the Proterozoic Eastern
Ghats Belt, India based on recent petrological, geophysical and geochronological data …

For this study Nd, Sr and Pb isotope compositions were analyzed for ortho-and
paragneisses from the Eastern Ghats Belt of India in order to determine its crust formation …

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 …