Results 141 to 150 of about 180 (171)

Partial Melting of Plagioclase-Free Garnet–Two-Mica Metapelite As a Model of the Formation of Ultra-Potassic Felsic Magmas under Conditions of the Continental Crust

Doklady Earth Sciences, 2023
O G Safonov, Varlamov D A, Van Reenen D D   +2 more
exaly  

Magma contamination in Himalayan leucogranite by metapelite host rocks: insights from chemical and boron isotopic compositions of tourmaline

International Geology Review, 2023
exaly  

Contrasting fertility of metapelite vs diorite gneiss to produce leucogranite melts: Example from the Mahalapye Complex, eastern Botswana

Journal of African Earth Sciences, 2022
Clarisa Vorster, G A Belyanin, H M Rajesh   +2 more
exaly  

Microstructural development in ductile deformed metapelitic-metapsamitic rocks

2015
The Pringles Metamorphic Complex, located in the central sector of the Sierra de San Luis, Argentina, is characterized by a several kilometers wide ductile shear zone developed over a geothermal gradient variable between greenschist and granulite facies.
Delpino, Sergio, Rueda, Marina, Urraza, Ivana, Grasemann, Bernhard   +3 more
openaire   +1 more source

Light element distribution in an amphibolite-facies metapelite

Geochimica et Cosmochimica Acta, 2006
Gieré, Reto, Jeffries, Teresa E., Garcia-Sanchez, R., Williams, C. Terry   +3 more
openaire   +2 more sources

High-pressure melting of metapelite and the formation of Ca-rich granitic melts in the Namche Barwa Massif, southern Tibet

Gondwana Research, 2012
Lingsen Zeng, , Chunyan Dong
exaly  

Metapelites: Progressive Mineral Changes

1965
openaire   +1 more source

Petrology and U–Pb zircon dating of coesite-bearing metapelite from the Kebuerte Valley, western Tianshan, China

Journal of Asian Earth Sciences, 2013
Lifei Zhang, Zuolin Tian
exaly  

Critical element mobilisation during metapelite melting and retrogression

The increasing demand for Li, Be, Cs, Sn, Ta, and W – critical for green energies and technologies – requires a better understanding of what controls the genesis of these elements’ deposits. Peraluminous granitoids – these elements’ main deposits – are formed through the melting of metapelites.
openaire   +1 more source

A long-lived tectono-metamorphic event in the late Paleoproterozoic: Evidence from SIMS U–Th–Pb dating of monazite from metapelite in central-south Trans-North China Orogen

Precambrian Research, 2020
Jia-Hui Liu, Hong-Xu Chen, Chun-Ming Wu   +2 more
exaly