A-type Granite
Chemical Process (Liquid-phase Growth) - Closed system under ground (Melt precipitation)
Synonym
Alkali granite, Alkaline granite
Definition
Igneous rocks with equigranular texture having mineral compositions as follows: Quartz in felsic minerals = 10-60 vol%, Plagioclase in feldspar = 10-65 vol%. A-type granite is determined by high (Na2O + K2O) / Al2O3. Other characters summarized below are those of general granites, and the rock type may be inferred but cannot be determined by mafic mineral assemblages.
Index Minerals
Annite, Hedenbergite, Hastingsite, Fayalite, Aegirine, Arfvedsonite, Riebeckite
Mineral composition
Mafic minerals < 30 vol% (Felsic), Quartz in felsic minerals = 10-60 vol%, Plagioclase in feldspar = 10-65 vol%.
Chemical composition
SiO2 > 66 wt% (Acidic), Na2O < 3.2 wt%
High (Na2O + K2O) / Al2O3, High Fe / Mg, and rich in F.
Texture
Granite: Equigranular texture composed of grains more than a few mm.
Granite porphyry, Quartz porphyry: Equigranular texture composed of grains more than a few mm, associated with larger euhedral phenocrysts.
Required Geological Setting
Occurrence
Rock forming minerals in A-type granites, felsic (acidic) plutonic rock formed from magma under ground. A-type Granites are anorogenic, and distribute as stocks in continental rift zones and hot spots. A-type Granites are included in ilmenite series. Distribution of A-type granites in Japan is very limited locations such as Cape Ashizuri (Kochi pref.), Iwaki island (Ehime pref.), and Lake Aoki (Nagano pref.).
Distribution of granites described in this site. Red is ilmenite-series granites corresponding to S-type granites, and blue is magnetite-series granites corresponding to I-type granites.
Mineral Assemblages
Quartz, Perthitic potassic feldspar, Plagioclase, Annite (Green), Hedenbergite, Hastingsite, Fayalite, Aegirine, Arfvedsonite, Riebeckite, Astrophyllite
Localities
- Cape Ashizuri (Pluton)
- Lake Aoki (Pluton)
- Iwaki island (Aegirine syenite)