The basaltic lavas erupted throughout the Mojave Desert are basanites (Si0~<46%, normative nepheline>5%, and K~0>1.5%), alkali-olivine bas~lts (Si0~46--48%; ne= 0--5% ; and K~O = 1.0--1.5%), and low-alumina, sub-alkaline basalts (SiO~ =48--51% ; ne ~ 0; K20< 1.0%). One volcano, Pisgah Crater, erupte
โฆ LIBER โฆ
The origin of fassaitic augite in the alkali basalt suite of the Hocheifel area, Western Germany
โ Scribed by H. G. Huckenholz
- Publisher
- Springer
- Year
- 1973
- Tongue
- English
- Weight
- 723 KB
- Volume
- 40
- Category
- Article
- ISSN
- 0010-7999
No coin nor oath required. For personal study only.
โฆ 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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