Mechanical properties and durability of slag granite geopolymer cement incorporated zirconium aluminum layered double hydroxide. [PDF]
Hashem FS, Salam ATA, Monir D.
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Petrographic and geochemical study of Precambrian and Paleozoic rocks in the western Anti-Atlas belt, Morocco: Facies, weathering, provenance and economic exploitation. [PDF]
Sebbab MM +10 more
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Integration of geophysical and remote sensing data for structural analysis and delineation of gold, fluorite, and barite mineralization in the Dawi shear belt, Egypt. [PDF]
Eldosouky AM +6 more
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Lithological discrimination based on Landsat-9 OLI sensor and field observation data: The bana an-orogenic volcano-plutonic ring complex, West Cameroon line. [PDF]
Mohamed R +4 more
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Fractal analysis of quartz boundaries as a strain rate proxy for tracing Earth's stress history. [PDF]
Abdolzadeh M +3 more
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Himalayan "S-type" granite generated from I-type sources. [PDF]
Ding H, Zhang Z, Kohn MJ.
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Integration of β-VAE, DWT, and GMM for Sentinel-2-based mapping of hydrothermal alteration and iron speciation in the Zafarghand area, Iran. [PDF]
Kalkhoran SE, Ghannadpour SS.
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The Lottah Granite is a composite pluton of tin-mineralised, strongly peraluminous alkali-feldspar granite which intrudes the Poimena Granite, a major component of the mid-Devonian Blue Tier Batholith of northeastern Tasmania. Earlier workers interpreted the Lottah Granite as a metasomatised differentiate of the Poimena Granite.
Lance P Black
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Abstract Granitoids are the dominant component of the continental crust and can be used as probes for crustal formation and evolution. The origin of granites, especially ambiguous granites with alkaline affinities emplaced in orogenic settings, however, remains controversial.
Guangxi Kuang +5 more
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Abstract Peralkaline to marginally metaluminous alkali-feldspar syenites and quartz alkali-feldspar syenites are hosted by subalkaline, ferroan rapakivi granites in the 1644 Ma Suomenniemi complex of southeastern Finland. These alkali syenites form NW-oriented dikes and small ( 99 and Or 90–100 Ab 0–10 ) and hypersolvus (Or 40–60 Ab 40–60 ) feldspar
E Suikkanen, O T Ramó
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