Search results for "Anorthite"
showing 3 items of 3 documents
Volatile dilution during magma injections and implications for volcano explosivity
2016
Magma reservoirs underneath volcanoes grow through episodic emplacement of magma batches. These pulsed magma injections can substantially alter the physical state of the resident magma by changing its temperature, pressure, composition, and volatile content. Here we examine plagioclase phenocrysts in pumice from the 2014 Plinian eruption of Kelud (Indonesia) that record the progressive capture of small melt inclusions within concentric growth zones during crystallization inside a magma reservoir. High-spatial-resolution Raman spectroscopic measurements reveal the concentration of dissolved H2O within the melt inclusions, and provide insights into melt-volatile behavior at the single crystal…
Mechanism of crystallization of pyroxene-based glass-ceramic glazes
2004
Abstract The mechanism of crystallization of a powdered glass with composition in the pyroxene crystallization primary field within the CaO–MgO–Al 2 O 3 –SiO 2 quaternary system and containing some additives was studied. The crystallization sequence was compared with that from the same base glass without additives. After a short thermal anneal both powdered glasses showed phase separation. Further thermal treatment gave rise to the crystallization of pyroxene. Anorthite as secondary crystalline phase was also detected in the quaternary glass (without additives). The starting crystallization in the glass with additives took place in the outer surface of glass particles probably in the immisc…
Microstructural and magnetic characterization of dusts from a stone crushing industry in Birbhum, India
2010
Abstract Stone dust sample collected from a stone crushing industry situated at Muhammad Bazar in Birbhum, India, is studied for its physical characterization using various techniques. Morphology and compositional analysis of the stone dust by scanning electron microscopy (SEM) reveal that the dust is an agglomeration of many tiny particles (0.32–2.12 μm), mostly having sharp edges, as well show microstructure heterogeneity. Elements present in the sample are detected by energy dispersive X-ray spectrometry (EDX). The X-ray diffraction (XRD) pattern analysis shows that the sample mainly contains minerals like anorthite, augite, esseneite and albite. An overall antiferromagnetic interaction …