Volcanic glass in Cretaceous dacites and rhyolites of the Paraná Magmatic Province, southern Brazil: Characterization and quantification by XRD-Rietveld
Autor: | Liza Angelica Polo, Flavio Machado de Souza Carvalho, Fábio Ramos Dias de Andrade, Valdecir de Assis Janasi |
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Rok vydání: | 2018 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences CRETÁCEO Geochemistry Mineralogy engineering.material 010502 geochemistry & geophysics Dacite Sanidine 01 natural sciences Cristobalite Volcanic glass Volcanic rock Geophysics Devitrification Geochemistry and Petrology Rhyolite engineering Plagioclase Geology 0105 earth and related environmental sciences |
Zdroj: | Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual) Universidade de São Paulo (USP) instacron:USP |
ISSN: | 0377-0273 |
Popis: | Acidic rocks are a significant component of the Cretaceous Parana Magmatic Province, occurring in different stratigraphic positions, and often forming deposits of complex and as yet poorly defined architecture. Vitrophyric varieties are surprisingly abundant for a volcanic sequence of this age, and are composed of predominant glass plus plagioclase (labradorite-andesine), pyroxenes (augite ± pigeonite and orthopyroxene), Ti-rich magnetite, and traces of apatite. Hypocrystalline rocks, largely derived from devitrification, additionally contain sanidine, cristobalite, and quartz. The negative correlation between the abundance of these minerals and the amount of glass suggests that these latter phases formed by devitrification. Modal analysis using a combined XRD Rietveld-RIR method detected glass contents between 0 and 85 wt% % in a set of representative samples of Palmas-type acidic rocks from southern Brazil with dacite to rhyolite composition. Modal compositions determined by XRD and by scanning electron microscope are in good agreement with each other, and were checked against whole-rock XRF chemical data. Water contents up to 4 wt% show a positive linear correlation with the amount of glass, and are inferred to be mostly secondary, as original (pre-eruptive) H2O dissolved in melts is inferred to have been |
Databáze: | OpenAIRE |
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