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The origin of fassaitic augite in the alkali basalt suite of the Hocheifel area, Western Germany

โœ Scribed by H. G. Huckenholz


Publisher
Springer
Year
1973
Tongue
English
Weight
723 KB
Volume
40
Category
Article
ISSN
0010-7999

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โœฆ Synopsis


Fassaitic augite (augite 3) occurs in elinopyroxenite fragments with cumulus textures or as anhedral crystals in alkali basalts and nepheline basanites of the Hocheifel Area. Rimming of augite 3 by phenocrystic augite (augite 2) followed by groundmass augite (augite 4) defines the sequence of the clinopyroxene crystallization. Fassaitic augites from other alkalibasalt series reveal clinopyroxene crystallization trends of increasing ferriTschermak's molecule and concomitant acmite as fractionation proceeds. This trend appears to be much more common than previously assumed.


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