Results 111 to 120 of about 199 (173)
Testing the stress-gradient hypothesis at the roof of the world: effects of the cushion plant Thylacospermum caespitosum on species assemblages. [PDF]
Dvorský M +7 more
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Pre-Variscan evolution of the Western Tatra Mountains: new insights from U-Pb zircon dating. [PDF]
Burda J, Klötzli U.
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High diversity and morphological convergence among melanised fungi from rock formations in the Central Mountain System of Spain. [PDF]
Ruibal C, Platas G, Bills GF.
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Siderophile Elements in Tracing Planetary Formation and Evolution. [PDF]
Walker RJ.
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Lithos, 2002
In the Higher Himalaya of the region from Cho Oyu to the Arun valley northeast of Makalu, the Miocene leucogranites are not hosted only in the upper High Himalayan Crystallines (HHC); a network of dykes also cuts the lower HHC and the Lesser Himalayan Crystallines (LHC).
Dario Visona, Bruno Lombardo
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In the Higher Himalaya of the region from Cho Oyu to the Arun valley northeast of Makalu, the Miocene leucogranites are not hosted only in the upper High Himalayan Crystallines (HHC); a network of dykes also cuts the lower HHC and the Lesser Himalayan Crystallines (LHC).
Dario Visona, Bruno Lombardo
exaly +4 more sources
Identifying xenocrystic tourmaline in Himalayan leucogranites
American Mineralogist, 2023Abstract Tourmaline is a common autocrystic mineral in granitic and pegmatitic rocks that records valuable information on the physicochemical evolution of magmas. However, xenocrystic tourmaline that does not crystallize from host magmas is also common but seldom reported and notoriously difficult to identify.
Jinsheng Han +4 more
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Petrochemical characteristics of leucogranite and a case study of Bengbu leucogranites
Science Bulletin, 2009Leucogranites have a relatively narrow variation in SiO2 content (70.5%–75.5%). Giving similar SiO2 content, leucogranites have relatively higher Al2O3 (>13.5%) and lower TFeO + MgO (
SuShu Guo, ShuGuang Li
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Experimental Crystallization of Leucogranite Magmas
Journal of Petrology, 1995Abstract Both crystallization and melting experiments have been carried out on two natural, biotite-muscovite (DK) and tourmaline-muscovite (GB) High Himalayan leucogranites (HHL) at 4 kbar, logfO2 = FMQ−0·5, aH2O = 1−0⋅03, and at five temperatures between 803 and 663°C H2O contents of the quenched glasses were analysed by ion ...
BRUNO SCAILLET +2 more
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