A re-examination of the typology of peraluminous
granite types in intracontinental orogenic belts.
All four of the dated samples fall in the peraluminous
Analysis revealed that these rocks have high K calc-alkaline affinity, whereas high alumina to silica ratio in these rocks infers them to be metaluminous to peraluminous
Mafic microgranular enclaves (MMEs) are common in metaluminous to peraluminous
granitoid plutons (Cantagrel et al.
1999): Mafic precursors, peraluminous
granitoids, and late lamprophyres in the Avila batholith, A model for the generation of Variscan batholiths in Iberia.
Petrogenesis of highly fractionated I-type peraluminous
granites: La Pedriza pluton (Spanish Central System).
1983), and b) Miocene peraluminous
garnet and two-mica-bearing granites which formed a section along the Baltoro glacier (Debon et al.
Nature of biotites from alkaline, calc-alkaline, and peraluminous
Mafic precursors, peraluminous
granitoids, and late lamprophyres in the Avila batholith: A model for the generation of Variscan batholiths in Iberia.
Postcollisional strongly peraluminous
granites, Lithos 45(1-4), 29-44.
Other topics of the 14 papers include translocation of heavy metals in Chinese cabbage, uranium in the water of abandoned mines, recent advances in separating uranium from other heavy metals, and uranium minerals from a Portuguese variscan peraluminous
Within the peraluminous
granitic rocks of southern Nova Scotia, uranium concentrations generally increase and thorium concentrations decrease with increasing magmatic differentiation, resulting in abnormally high eU/eTh associated with the most evolved parts of these granitic intrusions.