Shallow, texturally complex granites can be associated, spatially and temporally, with
hydrothermal alternation and mineralization. The formation of a granite-related ore deposit …

Epidote-group minerals rich in rare earth elements (REE), in particular allanite, are common
accessory phases in igneous, metamorphic, metasomatic, and sedimentary rocks. Small …

More than 5000 km 3 of nearly compositionally homogeneous crystal-rich dacite (∼ 68 wt%
SiO 2:∼ 45% Pl+ Kfs+ Qtz+ Hbl+ Bt+ Spn+ Mag+ Ilm+ Ap+ Zrn+ Po) erupted from the Fish …

Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by
Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude “ …

An extensive electron microprobe survey of amphibole compositions in the Fish Canyon
magma (2146 analyses), more than 80% of which are from high-resolution (< 10 μm steps) …

Ciomadul is the youngest volcano in the Carpathian–Pannonian region produced crystal-
rich high-K dacites that contain abundant amphibole phenocrysts. The amphiboles in the …

Abstract The Soursat Complex in northwestern of Iran is part of the Sanandaj-Sirjan
metamorphic belt. Three granitoid suites are present: Type I-syenogranite and deformed …

The Oetmoed Granite–Migmatite Complex (OGMC), Central Damara Orogen, Namibia,
consists mainly of∼ 526 to∼ 516 Ma garnet-and cordierite-bearing granite and …

Leucocratic A-type granites of the Proterozoic Damara orogen, Namibia are a distinctive
groups of rocks based on their mineralogical, chemical and isotopic characteristics. A-type …

ABSTRACT The Berens River area is representative of a broad belt of Archean felsic
plutonic rocks in the northwestern Superior Province of Ontario. The plutonic belt (Berens …