Oligoclase occurs, often accompanying orthoclase, as a constituent of plutonic igneous rocks such as granite, syenite, and diorite.
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This is coloured yellow brown to pink and contains fine crystals of perthite, and oligoclase and quartz, coloured by limonite.
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The mineral content and elemental abundance indicates " Jake M " rock may be a mugearite, a sodium rich oligoclase-bearing basaltic trachyandesite.
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The feldspar which usually displays the aventurine appearance is oligoclase, though the effect is sometimes seen in orthoclase : hence two kinds of sunstone are distinguished as " oligoclase sunstone " and " orthoclase sunstone ."
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The feldspar which usually displays the aventurine appearance is oligoclase, though the effect is sometimes seen in orthoclase : hence two kinds of sunstone are distinguished as " oligoclase sunstone " and " orthoclase sunstone ."
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This leads via the replacement of primary K-feldspar ( perthitic and non-perthitic microcline ) to the formation of plagioclase ( albite or oligoclase ) and in certain places also to the formation of myrmekite.
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For example, the plagioclase feldspars comprise a continuous series from sodium-rich end member albite ( NaAlSi 3 O 8 ) to calcium-rich anorthite ( CaAl 2 Si 2 O 8 ) with four recognized intermediate varieties between them ( given in order from sodium-to calcium-rich ) : oligoclase, andesine, labradorite, and bytownite.
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