Results 101 to 110 of about 798 (184)
Cordierite-orthoamphibole rocks associated with contrasting polymetallic mineralization occur in a wide range of metamorphic conditions in the Atik Lake, Manitoba, and Nemiscau and Montauban, Quebec, metamorphic terranes.Lithogeochemistry and ...
Bernier, Louis, 1961-
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Archean eclogite-facies oceanic crust indicates modern-style plate tectonics. [PDF]
Ning W, Kusky T, Wang L, Huang B.
europepmc +1 more source
The Ruby Range is one of several uplifted Precambrian blocks in southwest Montana, near the northwestern margin of the Archean Wyoming province. It was metamorphosed during the Big Sky orogeny ~ 1.72-1.79 Ga (Baldwin et al., 2014; Cramer et al., 2013 ...
Hamelin, Clémentine
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Geothermobarometry of Sahneh, Harsin-Nourabad ultramafic rocks (NE-Kermanshah) [PDF]
A Moradpour +4 more
openaire +1 more source
Miocene arc volcanism is manifested widely in the Valle del Cura-El Indio belt region (29°30´–30° South latitude), in the southern Central Andes of Argentina and Chile.
V.D. LITVAK, S. POMA
doaj
Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway. [PDF]
Dunkel KG, Morales LFG, Jamtveit B.
europepmc +1 more source
Massive methane fluxing from magma-sediment interaction in the end-Triassic Central Atlantic Magmatic Province. [PDF]
Capriolo M +11 more
europepmc +1 more source
The southern Alaska margin is a complex geologic region with a history of subduction-accretion, plutonism, and metamorphism. The Chugach–Prince William accretionary terrane (CPW) is intruded by the Sanak-Baranof plutonic belt, a series of intrusions ...
Boyle, Claire
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Química mineral, geotermobarometria e suas implicações na evolução do Complexo Pinheiro Machado, região de Monte Bonito, RS [PDF]
Este trabalho apresenta dados de petrologia, química mineral e de geotermobarometria das rochas do Complexo Pinheiro Machado na região de Monte Bonito, domínio oriental do Cinturão Dom Feliciano. Os dados foram obtidos a partir de estudos petrográficos e
Bastos, Vivianne Andrade
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The quantitative pressure (P)–temperature (T) conditions of low-grade metamorphic rocks, such as pumpellyite–actinolite and greenschist facies, are largely unknown mainly owing to the difficulty in applying thermodynamic methods despite their
Yuki Tomioka +2 more
core +1 more source

