Results 101 to 110 of about 5,714 (221)
Continental crust forms in magmatic arcs and transforms through collision, as seen in the Tibetan crust shaped by Neo‐Tethyan subduction and India‐Asia collision.
Wen‐Rui Sun +4 more
doaj +1 more source
Heat transfer by fluids in granulite metamorphism
The thermal role of fluids in granulite metamorphism was presented. It was shown that for granulites to be formed in the middle crust, heat must be advected by either magma or by volatile fluids, such as water or CO2.
Morgan, Paul, Ashwal, Lewis D.
core
Low H2O activity of fluid in mafic granulite in far-eastern Nepal (forecast)
2012-03The P-T-XH2O condition of mafic granulite in far-eastern Nepal has been investigated using multi-equilibrium thermobarometry. Based on retrograde zoning in amphiboles and the amphibole + plagioclase symplectite surrounding garnet and clinopyroxene,
今山, 武志, Imayama, Takeshi
core +1 more source
Granulite-facies metamorphism in the structurally lower part of the Saxon Granulite Massif ...
Romer, Rolf L. (Prof. Dr.) +1 more
core
Granulite Facies Metamorphism in the Coast Range Crystalline Belt
Mineral assemblages diagnostic of the granulite facies of metamorphism occur between Terrace and Prince Rupert, British Columbia. The estimated pressure (5–8 kb) and temperature (750–850 °C) of metamorphism are important constraints in unravelling the ...
Lincoln S. Hollister
core +1 more source
Sm-Nd garnet and U-Pb zircon ages for eclogite and granulite from the Breaksea Orthogneiss provide a detailed chronology for pluton emplacement and subsequent thermal history of the lower arc crust exposed in Fiordland, New Zealand.
Stowell, Harold H. +5 more
core
The ~1 Ga Oaxacan Complex is the largest exposure of the Oaxaquia terrane of Mexico. Microprobe analysis of co-existing ortho- and clino-pyroxene, garnet, ilmenite and plagioclase indicate metamorphic conditions of 735 ± 5° C and 7.7 ± 0.1 kbar in the ...
Luigi A. Solari +4 more
doaj
Partial melting. granulite facies metamorphism and the evolution of the continental crust
Partial melting. granulite facies metamorphism and the evolution of the continental crust. The basement of the continents is made up largely of rocks that have partially melted at deep levels in ancient mountain belts.
core
Influence of Measurement Uncertainty in the Determination of Selected Rock Parameters-A Realistic Approach. [PDF]
Voit K +4 more
europepmc +1 more source
Copper isotope evidence for sulfide fractionation and lower crustal foundering in making continental crust. [PDF]
Liu SA +5 more
europepmc +1 more source

