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- Plagioclase - Wikipedia
Plagioclase is a major constituent mineral in Earth's crust and is consequently an important diagnostic tool in petrology for identifying the composition, origin and evolution of igneous rocks Plagioclase is also a major constituent of rock in the highlands of the Moon
- Plagioclase Feldspar: A group of common rock-forming minerals
What is Plagioclase? Plagioclase is the name of a group of feldspar minerals that form a solid solution series ranging from pure albite, Na (AlSi 3 O 8), to pure anorthite, Ca (Al 2 Si 2 O 8) Minerals in this series are a homogenous mixture of albite and anorthite
- Plagioclase: Mineral information, data and localities.
In petrology, the plagioclase series are defined based on their percentage of the two end-members albite (Ab) to anorthite (An) Compositions of individual samples are usually written as An24Ab76 meaning in this case that it is a solid-solution member consisting of 24% anorthite and 76% albite
- Plagioclase - ALEX STREKEISEN
The plagioclase series is arbitrarily divided into six minerals or compositional ranges: albite (Ab 90 - Ab 100), oligoclase (Ab 70 - Ab 90), andesine (Ab 50 - Ab 70), labradorite (Ab 30 - Ab 50), bytownite (Ab 10 - Ab 30), and anorthite (Ab 0 - Ab 10)
- Plagioclase Mineral Data
Igneous and metamorphic rocks Group name for Na, Ca feldspars Common world wide occurrences Link to MinDat org Location Data From the Greek plagios - "oblique" and klao - "I cleave" in allusion to the obtuse cleavage angles of the good cleavages
- Plagioclase - Geology is the Way
Plagioclases are fundamental constituents of the Earth’s crust and also of the anorthosite crust of the Moon (the highlands) The name plagioclase derives from the Greek πλάγιος (plágios, “oblique”) + κλᾰ́σῐς (klásis, “fracture”), in reference to its two cleavage systems
- Plagioclase | Definition, Uses, Facts | Britannica
Plagioclase, any member of the series of abundant feldspar minerals usually occurring as light-colored, glassy, transparent to translucent, brittle crystals Plagioclase is a mixture of albite, or sodium aluminosilicate, and anorthite, or calcium aluminosilicate
- Plagioclase Feldspar | Common Minerals
Plagioclase minerals are hard, non-metallic minerals that exhibit two cleavage directions that meet at nearly right angles The name ‘plagioclase’ refers to this cleavage pattern, coming from the Greek words for ‘oblique’ (plagios) and ‘to break’ (klasis)
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