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Compositional Zoning of Spessartine-Grossular Garnets in the Archean Metavolcanics of the Central Bundelkhand Greenstone Complex, Bundelkhand Craton, Indian Shield
The paper deals with the peculiarities of the chemistry and internal structure of garnet from the Archean metavolcanites of the Mauranipur structure...
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Mineralogical Characteristics and Magmatic Evolution Significance of Garnets in the Late Jurassic Granites in **ngcheng, Eastern North China Craton
AbstractA series of Mesozoic granites related to the subduction of the ancient Pacific plate are widely developed in the eastern part of the North...
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Sulfide anatexis during high-grade metamorphism: a case study from the Bodenmais SEDEX deposit, Germany
Many sedimentary-exhalative (SEDEX) sulfide deposits have been subject to regional metamorphism and, if the metamorphic grade was high enough, this...
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An Experimental Study of Partial Melting of Metafelsic Rocks: Constraints on the Feature of Anatectic Melts and the Origin of Garnets in Collisional Orogens
Crustal anatexis in continental subduction zones has great bearing on chemical differentiation of the continental crust at convergent plate...
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Typomorphic Features of Garnets and Zircons from the Middle Neopleistocene Moraines in the Northern and Southern Timan–Pechora–Vychegda Region
AbstractThe typomorphism and chemical composition of garnets and zircons were studied in the Pechora (Dnieper) and Vychegda (Moscow) Middle...
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Garnet EoS: a critical review and synthesis
All available volume and elasticity data for the garnet end-members grossular, pyrope, almandine and spessartine have been re-evaluated for both...
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The potential for using metagreywacke to study metamorphism of amphibolite facies conditions: a comparison study within the Luminárias Nappe, Southern Brasília Orogen (Southeastern Brazil)
Metagreywacke is a very common rock type in orogenic settings. It occurs in several domains within the Neoproterozoic Southern Brasília Orogen, that...
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Mineral chemistry and monazite chemical Th–U–total Pb dating of the Wadi Muweilha muscovite pegmatite, Central Eastern Desert of Egypt: constraints on its origin and geodynamic evolution relative to the Arabian Nubian Shield
The Wadi Muweilha muscovite pegmatite in the Central Eastern Desert (CED) of Egypt is strongly influenced by a strike-slip shearing and fault system...
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Generation of multiple low-K granitic magmas in the eastern Qilian orogen, NE Tibetan Plateau: implications for granite genesis and pluton construction
Granite genesis is crucial to understanding the evolution of continental crust, yet many concerns about granite genesis remain not well answered,...
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Metamorphic P–T conditions and ages of garnet-biotite schists in the Dahongshan Group from the southwestern Yangtze Block
The Dahongshan Group, situated at the southwestern margin of the Yangtze Block, represents a geological unit characterized by relatively high-grade...
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Tracing fluid infiltration into oceanic crust up to ultra-high-pressure conditions
Fluid–rock interaction within the altered oceanic crust and across the slab–mantle boundary during subduction facilitates element transfer, but the...
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Geochemistry and mineral chemistry of granitic rocks from west Wadi El Gemal area, southern Eastern Desert of Egypt: Indicators for highly fractionated syn- to post-collisional Neoproterozoic felsic magmatism
Leucogranite, pegmatite, and aplite from selected areas in the Wadi El Gemal area in the southern Eastern Desert of Egypt were investigated...
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Cambro-Ordovician metamorphism from Lesser Himachal Himalaya and its implication for Gondwana assembly
As a tectonic window into the Lesser Himachal Himalaya, India, a group of metasediments and gneissic rocks, known as the Jutogh Group and Wangtu...
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Low-pressure isobaric cooling metamorphic P–T paths from Botnnuten in the southern Lützow-Holm Complex, East Antarctica
This paper reports the metamorphic texture of cordierite megacrysts and the metamorphic P–T path of a newly exposed section of gneiss in East...
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Variations in orientation relationships between rutile inclusions and garnet host relate to magmatic growth zoning
Rutile inclusions in almandine-spessartine garnet from a peraluminous pegmatoid from the Moldanubian zone (Bohemian Massif, AT) show distinct changes...
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The Genesis of the Kenticha rare-metal granite-pegmatite, Southern Ethiopia
The Kenticha pegmatite field comprises suites of barren to fertile pegmatite swarms. It shows textural, mineralogical, and geochemical variations....
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Remote sensing techniques and geochemical constraints on the formation of the Wadi El-Hima mineralized granites, Egypt: new insights into the genesis and accumulation of garnets
The Wadi El-Hima Neoproterozoic I- and A-type granites in the Southern Eastern Desert of Egypt are rich in garnets (up to 30 vol%) and are cut by...
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The Paleozoic Huoshenmiao iron skarn deposit in the Tongbai area of North Qinling Orogen, China: Insights from garnet U-Pb dating and geological constraints
The Qinling Orogen is a composite orogenic belt that can be subdivided into the North and South Qinling, broadly separated by the Shangdan suture...
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Hosts of Sn in reduced deep-seated W skarn systems: A case study on the world-class scheelite skarn deposit, Zhuxi, South China
Tin (Sn) and tungsten (W) behave incompatibly in reduced magmatic systems and may become enriched in late highly-evolved melts. Nonetheless, Sn and W...
