Results 151 to 160 of about 452 (179)
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Accessory Fe-Ti oxides in the West-Carpathian I-type granitoids: witnesses of the granite mixing and late oxidation processes

Mineralogy and Petrology, 2011
Fe-Ti-oxides may reach hundreds ppm in I-type granitoids and close to microgranular mafic enclaves (MME) up to several thousands ppm. Western Carpathian I-type granitoids have magnetic susceptibility above 3 × 10−4 SI units, whereas S-type granites are lower. Associated MMEs reach up to 160 × 10−4 SI. The measurement of magnetic susceptibility in field
Igor Broska, Igor Petrík
openaire   +1 more source

I-type plutonism in a continental back-arc setting: Miocene granitoids and monzonites from the central Aegean Sea, Greece

Contributions to Mineralogy and Petrology, 2002
Miocene extension in the Aegean Sea was accompanied by the intrusion of granitoid and monzonitic magmas at upper crustal levels. With increasing distance from the trench, the metaluminous to slightly peraluminous I-type intrusives show a systematic regional variation in their compositions: medium- to high-K granodiorites in the WSW, high-K low-silica ...
Altherr, R., Siebel, W.
openaire   +3 more sources

Triassic I-type granitoids from the Torbat e Jam area, northeastern Iran: Petrogenesis and implications for Paleotethys tectonics

Journal of Asian Earth Sciences, 2018
Abstract The closure of the Paleotethys ocean in the Tethyan orogenic belt in northeastern (NE) Iran, related to the collision between Gondwana-derived terranes in the south and Laurasia in the north, remains controversial due to the sparsity of Paleozoic ophiolitic outcrops but can be constrained by contemporaneous granitoids.
Jamal Ghavi   +3 more
openaire   +1 more source

Genesis of ilmenite-series I-type granitoids at the Baogutu reduced porphyry Cu deposit, western Junggar, NW-China

Lithos, 2016
Abstract The Baogutu porphyry Cu deposit is a typical reduced porphyry Cu deposit, likely related to ilmenite-series I-type granitoids. However, the nature of the granitoids (ilmenite-series or magnetite-series) and the genesis of the Baogutu deposit are still under debate.
Cao, M.   +5 more
openaire   +2 more sources

Cretaceous fractionated I-type granitoids and metaluminous A-type granites in SE China: the Late Yanshanian post-orogenic magmatism

Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 2000
The Late Yanshanian Orogeny (130-90 Ma) encompasses an important Mesozoic magmatic event in the crustal evolution of SE China. Products of post-orogenic magmatism, widely distributed in the eastern part of Zhejiang and Fujian provinces known as the Southeast Coast Magmatic Belt (SCMB), are dominated by large amounts of slightly Nb and Ta depleted, high-
Cheng-Hong Chen   +5 more
openaire   +1 more source

MAGMATIC MELANOCRATIC INCLUSIONS IN I-TYPE GRANITOIDS

International Geology Review, 1989
P. V. Yermolov   +4 more
openaire   +1 more source

EMPLACEMENT LEVELS OF DEVONIAN I-TYPE GRANITOIDS OF THE PISCATAQUIS MAGMATIC BELT, CENTRAL AND WESTERN MAINE

Geological Society of America Abstracts with Programs, 2019
Sean Brock, David Gibson
openaire   +1 more source

On the petrology and microstructures of small-scale ductile shear zones in granitoid rocks: An overview

Journal of Structural Geology, 2022
Alberto Ceccato   +2 more
exaly  

222Rn Concentration in Groundwaters Circulating in Granitoid Massifs of Poland

Water (Switzerland), 2020
Agata Kowalska, Tadeusz A Przylibski
exaly  

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