Results 61 to 70 of about 52,304 (124)

Zinc Contents of Mafic Micerals in Granitic Rocks, with Special Reference to Ore Chemistry [PDF]

open access: yes, 2003
In order to know the reason why the Cu/Zn-Pb ratios of skarn-type deposits related with the ilmenite-series granitic rocks are markedly higher than those related with the magnetite-series, comparative mineralogical studies were carried out for the two ...
Inoue, Yoshinori   +2 more
core   +1 more source

Top-down structures of mafic enclaves within the Valle Fértil magmatic complex (Early Ordovician, San Juan, Argentina)

open access: yes, 2021
Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have been studied in the Valle Fértil calc-alkaline igneous complex, Argentina.
Martino, Roberto Donato   +7 more
core  

"Mineral and whole-rock geochemistry of Kestanbol Pluton (Ezine-Çanakkale) and their mafic microgranular enclaves, NW Anatolia-Turkey: Some evidences of felsic and mafic magma interaction."

open access: yes, 2010
:     The Miocene Kestanbol granitoid, in Ezine-Canakkale, Turkey, is one of post-collision granitoids of western Anatolia, which have been related to the the late Cretaceous collision between the Anatolide-Tauride platform and the Pontides ...
YILMAZ ŞAHİN, SABAH   +5 more
core  

Top-down structures of mafic enclaves within the Valle Fértil magmatic complex (Early Ordovician, San Juan, Argentina) [PDF]

open access: yes, 2009
Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have been studied in the Valle Fértil calc-alkaline igneous complex, Argentina.
PINOTTI, Eleonora   +7 more
core  

Model for the Origin and Significance of Microgranular Enclaves in Calc-alkaline Granitoids

open access: yes, 1991
The origin and significance of microgranular enclaves as indicators of the occurrence of magma mixing and/or mingling episodes between basic magmas and anatectic acid magmas, either I- or S-type, are re-evaluated.
POLI, Giampiero, S. Tommasini
core   +1 more source

Mafic enclaves record syn-eruptive basalt intrusion and mixing [PDF]

open access: yes, 2018
Mafic enclaves hosted by andesite erupted at the Soufrière Hills Volcano between 1995 and 2010 yield insights into syn-eruptive mafic underplating of an andesite magma reservoir, magma mixing and its role in sustaining eruptions that may be widely ...
Barclay, Jenni   +20 more
core   +2 more sources

Physico-mechanical properties of the system syenite-enclave in the Královec quarry

open access: yes, 2017
The bachelor thesis focuses on mechanical properties of syenitoids and their mafic microgranular enclaves collected in actively mined quarry Královec near Jaroměřice nad Rokytnou.
Umlauf, Jiří
core   +1 more source

Interaction between felsic and mafic magmas in the Salmas intrusive complex, Northwestern Iran: constraints from petrography and geochemistry

open access: yes, 2015
The Salmas plutonic complex, in the northernmost part of Sanandaj-Sirjan Zone of Iran, provides evidence for magma interaction processes. The complex contains mafic-intermediate, hybrid and felsic rocks which intruded into the Paleozoic metamorphic ...
Peter Appel   +26 more
core   +1 more source

Fingerprinting feldstar phenocrysts using crystal isotopic composition stratigraphy:Implications for crystal transfer and magma mingling in S-type granites

open access: yes, 2000
Microsampling of cm-scale feldspar crystals within an S-type granite from the Lachlan Fold Belt of southeastern Australia has revealed complex internal Sr and Nd isotopic variations.
Waight, Tod E.   +2 more
core   +1 more source

Magma mixing in the Karamaili granite belt of Eastern Junggar: evidence from A2-type granites and their mafic microgranular enclaves [PDF]

open access: yes
The Karamaili Orogenic Belt forms an essential part of the southernmost margin of the Eastern Junggar Orogenic Belt. The Late Carboniferous granitic belt of the Karamaili belt provides a valuable natural setting for studying the evolution of silicic ...
Yuan Yao   +5 more
core   +1 more source

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