anorthite oor Portugees
anorthite
en
(mineralogy) A plagioclase feldspar, the final member of the Albite-Anorthite solid solution series. Anorthite is very rare on Earth, but abundant in moon rocks. This is because Anorthite weathers rapidly to clay minerals under atmospheric conditions. Good crystals have been found in lava-digested limestone blocks erupted from Mount Vesuvius.
Vertalings in die woordeboek Engels - Portugees
anortita
en
mineral
Anortita
en
mineral, Ca-feldspar, Ca-silicate, tectosilicate
anortite
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The series ranges from albite to anorthite endmembers (with respective compositions NaAlSi3O8 to CaAl2Si2O8), where sodium and calcium atoms can substitute for each other in the mineral's crystal lattice structure.
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Anorthite was named by Gustav Rose in 1823 from the Ancient Greek meaning oblique, referring to its triclinic crystallization.
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Chemical analysis of the Genesis Rock indicated it is an anorthosite, composed mostly of a type of plagioclase feldspar known as anorthite.
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It has an anorthite percentage (%An) of between 50 and 70.
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The chemical formula of pure anorthite is CaAl2Si2O8.
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The following table shows their compositions in terms of constituent anorthite and albite percentages.
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The composition of a plagioclase feldspar is typically denoted by its overall fraction of anorthite (%An) or albite (%Ab), and readily determined by measuring the plagioclase crystal's refractive index in crushed grain mounts, or its extinction angle in thin section under a polarizing microscope.
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In contrast to the Earth, large portions of the lunar crust appear to be composed of rocks with high concentrations of the mineral anorthite.
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Contents Plagioclase series membersEdit The composition of a plagioclase feldspar is typically denoted by its overall fraction of anorthite (%An) or albite (%Ab), and readily determined by measuring the plagioclase crystal's refractive index in crushed grain mounts, or its extinction angle in thin section under a polarizing microscope.
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The following table shows their compositions in terms of constituent anorthite and albite Andesine
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On the other hand, partial cryst (mais) allization of basalt fibers occurred at ~ 800oC, resulting in diffraction peaks in the X-ray patterns, characteristic of silicates and aluminosilicates as the anorthite from the plagioclase class.
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Anorthite was detected in diffraction X-ray analysis in GP, but its level should be limited for the low content of calcium in the batch.
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