Results 11 to 20 of about 52,304 (124)
A systematic data set of petrography, mineralogy, geochronology, and geochemistry is reported for typical arc granitoids and associated mafic microgranular enclaves (MME) from the Chinese Altai, Central Asian Orogenic Belt.
Xing Cui +4 more
doaj +2 more sources
Petrologic Reconstruction of Sulfur Transfer Processes During Mafic Magma Recharge: Insight From Anhydrite-Bearing Mafic Microgranular Enclaves [PDF]
Supplementary Tables S1-S6 for "Petrologic reconstruction of sulfur transfer processes during mafic magma recharge: Insight from anhydrite-bearing mafic microgranular enclaves".
Madeleine Humphreys +2 more
exaly +4 more sources
Paired host-enclave geochemistry of mafic microgranular enclaves in the Eastern Belt granite, Peninsular Malaysia [PDF]
This paper describes some of the important petrographic characteristics of the mafic microgranular enclaves and their host rock as well as their chemical relationship to selected granitic rocks from the Eastern Belt granite of Peninsular Malaysia. The enclaves are invariably darker coloured and finer grained than the enclosing granitic rocks.
Editor Geological Society of Malaysia
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Triaxial Compression Testing of Multicomponent Geomaterials from Quartz-Poor (Syenitic) Systems [PDF]
This paper focuses on mafic microgranular enclaves enclosed in quartz-poor igneous rocks and their effect on strength properties of the rock massif. The study examines host rock–enclave multicomponent geomaterials from enclave-bearing syenitic rocks from
Krmíček Lukáš, Závacký Martin
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The Miocene Kestanbol granitoid, in Ezine-Çanakkale, 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. Magmatism began during the early Miocene, with coeval alkaline to calc-alkaline plutonism and volcanism, controlled by
Sahin, Sabah Yilmaz +5 more
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Contribution from Mafic Melt to the Zhireken Porphyry Mo-Cu Deposit, Eastern Transbaikalia, Russia: Evidence from Mafic Microgranular Enclaves [PDF]
Mafic microgranular enclaves (MME) were formed in felsic ore-bearing porphyries from the Zhireken por-phyry Mo-Cu deposit, eastern Transbaikalia, Russia. Porphyry rocks were emplaced during the Upper Jurassic. Most of the enclaves are globular, oval-shaped and intermediate in composition (54% SiO2).
ANITA, N. BERZINA, VITALY, I. SOTNIKOV
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BACKGROUND The compositions of the bulk-rocks are commonly modified by hydrothermal alteration or merely represent the magmatic information of snapshot during evolution.
WANG Dan, FU Yong
doaj +1 more source
Interaction of the lithospheric mantle and crustal melts for the generation of the Horoz pluton (Niğde, Turkey): whole-rock geochemical and Sr–Nd–Pb isotopic evidence [PDF]
The Horoz pluton includes granitic and granodioritic rocks, with widespread mafic microgranular enclaves (MMEs). Petrochemically, the rocks of the pluton show calc-alkaline to shoshonitic and metaluminous to slightly peraluminous composition.
Kerim Kocak, Veysel Zedef
doaj +1 more source
Geosphere, April 2017, v. 13, p. 482-517, doi:10.1130/GES01407.1, Supplemental Table 3 - Hornblende compositions of the Permian granitoids and their mafic microgranular ...
Yue Zhao (186573) +1 more
core +3 more sources
Abstract The Miocene tectonics of Papua New Guinea, where subduction, arc-continent collision, and changes in subduction direction are considered to have occurred, is very complex and various tectonic models have been proposed. The Maramuni arc, active in the Miocene, is composed of a chain of granitoid bodies.
Hoshide Takashi +2 more
openaire +2 more sources

