Search results for "Chemical heterogeneity"

showing 3 items of 3 documents

Effects of natural radiation damage on back-scattered electron images of single crystals of minerals

2006

Generally, it has been assumed that signal intensity variations in back-scattered electron (BSE) images of minerals are mainly controlled by chemical heterogeneity. This is especially true for images of single crystals, where effects of different crystal orientations with respect to the incident beam on the observed BSE are excluded. In contrast, we show that local variations of the structural state within single-crystals (i.e., degree of lattice order or lattice imperfectness) may also have dramatic effects on the back-scattering of electrons. As an example, we present BSE images of single-crystals of natural zircon, ZrSiO 4 , whose intensity patterns are predominantly controlled by struct…

010504 meteorology & atmospheric sciencesCondensed matter physicsChemistryMineralogyElectron010502 geochemistry & geophysics01 natural sciencesStructural heterogeneityCrystalGeophysicsGeochemistry and PetrologyRadiation damageIncident beamSignal intensity0105 earth and related environmental sciencesZirconChemical heterogeneityAmerican Mineralogist
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Element variations in rhyolitic magma resulting from gas transport

2013

Tuffisite veins are glass-filled fractures formed when magma fragments during degassing within the conduit. These veins form transient channels through which exsolved gases can escape from magma. The purpose of this study is to determine the extent to which chemical heterogeneity within the melt results from gas transport, and assess how this can be used to study magma degassing. Two tuffisite veins from contrasting rhyolitic eruptions at Torfajökull (Iceland) and Chaitén (Chile) were studied in detail. The tuffisite vein from Torfajökull is from a shallow dissected conduit (~70. ka) that fed a degassed lava flow, while the sample from Chaitén was a bomb ejected during the waning phases of …

010504 meteorology & atmospheric sciencesLavaDiffusionGeochemistryMineralogy010502 geochemistry & geophysics01 natural sciences13. Climate actionGeochemistry and PetrologyMagmaRhyolitecardiovascular systemParticleVein (geology)VolatilesGeology0105 earth and related environmental sciencesChemical heterogeneityGEOCHIMICA ET COSMOCHIMICA ACTA
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Melt extraction and accumulation from partially molten rocks

2004

Current models for melt segregation and ascent are not adequate to accurately describe transport and accumulation in combination. We propose that transport is discontinuous and in batches, and that accumulation occurs by stepwise merging of batches. A simple numerical model of jostling spheres that merge when they touch was used to represent stepwise accumulation and transport of batches by propagation of hydrofractures. Results of the numerical model indicate that such a system may quickly develop into a self-organised critical (SOC) state. In this state, the distribution of melt batch volumes can be described by a power law, with an exponent m that lies between 2/3 and 1. Once a self-orga…

geographygeography.geographical_feature_categoryPlutonMineralogyGeologyMagma chamberMigmatitePower lawVolcanic rockChemical evolutionGeochemistry and PetrologySPHERESGeologyChemical heterogeneityLithos
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