Results 11 to 20 of about 801 (184)
: The Cenozoic Himalayan leucogranite-pegmatite belt has been a hotspot for rare metal exploration in recent years. To determine the genesis of the pegmatite in the Himalayan region and its relationship with the Greater Himalayan Crystalline Complex (GHC)
Hua-wen Cao +8 more
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Abstract. The New Exploration Tools for European Pegmatite Green-Tech Resources (GREENPEG) spectral database contains the spectral signature, obtained through reflectance spectroscopy studies, of European pegmatites and minerals as well as their host rocks.
J. Cardoso-Fernandes +9 more
openaire +5 more sources
Research subject. The Mamskay muscovite province (MMP) is located on the border between the Siberian platform and the Baikal orogenic area, near the boundary fault. The MMP hosts numerous regional and local thrust and reverse faults, which are typical of
A. P. Kochnev, A. V. Cheremnykh
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Pegmatites in Sura and Verkhivtseve greenstone belts of the Middle Dnipro region, Ukrainian shield
Rare-metal granite pegmatites of the lithium-cesium-tantalum (LCT) type are widely distributed in Early Precambrian Greenstone belts worldwide, including the Canadian and Australian shields.
V. V. Sukach +4 more
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Gabal El Urf region is located in the northern Egyptian Eastern Desert and overlain essentially by older and younger granitoids of Late Proterozoic age.
Amr Abdel Hamid +3 more
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ON ESTIMATION OF VERTICAL AMPLITUDE OF VEIN PEGMATITE SERIES IN THE NORTHWESTERN BELOMORIE
The article is devoted to the problem of the vertical amplitude of the Belomorian vein fields’ pegmatite genesis which has not been characterized so far.
Николай Дмитриевич Малов +1 more
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Geochemical and Isotope Anomalies in Sioma River Gorge, Western Tajikistan
For a better understanding of the previously observed increased natural radioactivity at the confluence of the Varzob and Sioma rivers, Central Tajikistan, the activity concentration of natural radioactive 40K, Th and U daughters as well as of the ...
Djamshed A. Abdushukurov +3 more
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Fluid exsolution in magmas is a process that, in many silicic upper crustal reservoirs, starts at relatively low crystallinities (near liquidus), and precedes the precipitation of many ore bodies, including pegmatites.
Ludmila Maria Fonseca Teixeira +3 more
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The Sveconorwegian Pegmatite Province – Thousands of Pegmatites Without Parental Granites [PDF]
Abstract The Late-Proterozoic Sveconorwegian pegmatite province in southern Norway and southwest Sweden hosts seven rare-element pegmatite districts with more than 5000 rare-element pegmatites. Most of these pegmatites with Niobium-Yttrium-Fluorine (NYF) signature are not related to a parental granite, but instead occur in areas of high-grade ...
Müller, Axel +2 more
openaire +3 more sources
The existence of diagnostic features in the visible and infrared regions makes it possible to use reflectance spectra not only to identify mineral assemblages but also for calibration and classification of satellite images, considering lithological and ...
Joana Cardoso-Fernandes +9 more
doaj +1 more source

