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Examples ofdacitic
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The third stage includes the emplacement of severaldaciticdomes outside of the central crater and at different times.
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This is consistent with the major-element data and a primarily andesitic source, modified bydaciticand more felsic components.
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C9 member is a 500 m thick sequence of moderately dipping (20°), massive, highly welded crystal-richdaciticignimbrites.
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An alternative view holds that a very large crystalrichdaciticchamber may be the product of protracted growth of a shallow magma system that was never near its liquidus.
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Due to the compression of the magma chamber, basaltic lava rose from the bottom to the higherdaciticmagma chamber at 8 km deep.
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This example is from Wikipedia and may be reused under a CC BY-SA license.Thesedaciticmagmas may have evolved by the accumulation of multiple injections of mushy magma sustained over hundreds of thousands of years.
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It must be noted that this algorithm is mainly calibrated for basaltic todaciticmelts and that it is less accurate for granitic liquids.
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The majority of these are rhyolitic/dacitic/trondhjemitic and basaltic, commonly hosting massive sulphide deposits of economic importance.
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The eruptions started with production of rhyolitic magma followed bydaciticto basaltic andesite magma.
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Shortly before eruption, adaciticmagma has evolved into a water-rich melt laden with 40 to 50 % crystals.
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The evolution of adaciticmagma system over an approximately 1 million year time period is shown in this series of cross-sections.
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In contrast, monotonousdaciticmagmas may never have been crystal-free near-liquidus magmas.
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The roof collapses (e) and triggers eruption of the crystal-richdaciticmagma.
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Furthermore, the eruptive characteristics and inferred crystallization histories imply that this type of crystal-richdaciticmagma was never near its liquidus.
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It consists of weldeddaciticignimbrites, which lack quartz crystals and are further distinguished by zoned plagioclase crystal fragments.
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In contrast, most comparable deposits described from the geological record are typicallydacitic-rhyodacitic and contain rhyolitic glass.
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Daciticto andesitic basalts contain phenocrysts of pyroxene, altered feldspar and minor quartz often set in a groundmass of epidote-chlorite-glass.
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Eruption from such a chamber produces a deposit that isdaciticand somewhat variable in composition, but not systematically zoned.
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Several very large volume (> 1000 km of erupted magma) ignimbrites aredaciticand lack the vertical zonation found in many other tuffs.
From theCambridge English Corpus
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