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词汇 sanidine
释义 BETA

Examples of sanidine


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Phenocrysts include both quartz (10-15 %) and feldspar (10 %; mostly sanidine), both measuring about 2 mm in diameter on average.
For selected ignimbrites, sanidine crystals were taken from fresh, unaltered pumice lapilli.
Further refinement of the formation's age using radiometric dating of sanidine crystals has resulted in an age of 34 million years old.
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It commonly occurs in association with orthoclase, sanidine, labradorite, olivine, leucite, amphiboles and other pyroxenes.
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Phenocrysts are sodic sanidine with minor albite and bipyramidal quartz.
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This facies is named for the mineral sanidine.
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Other minerals in this group include adularia, anorthoclase, buddingtonite, celsian, hyalophane, microcline, monalbite, orthoclase, and sanidine.
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Due to the high temperature and rapid quenching, sanidine can contain more sodium in its structure than the two polymorphs that equilibrated at lower temperatures.
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Minerals typical of lamproites include: forsteritic olivine; high iron leucite; titanium-rich aluminium-poor phlogopite; potassium- and titanium-rich richterite; low aluminium diopside; and iron-rich sanidine.
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This structure is very similar to that of orthoclase and sanidine but differs in a couple of ways:: 1.
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The upper part contains sanidine, analcime, melanite and rock fragments.
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Crystals of euhedral sanidine and marginally corroded plagioclase reach up to 500 m in size and are usually extensively altered to kaolinite.
The lower part of the formation is trachytic with abundant sanidine phenocrysts, melanite and pyroxene.
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Sanidine is a polymorph of alkali feldspar stable at yet higher temperature.
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Pericline twinning is a type of crystal twinning which show fine parallel twin laminae typically found in the alkali feldspars sanidine, microcline and albite.
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