Western dome of the Arga-Ynnykh-Khaya granitic intrusion and its white granites

Adamellites, granite porphyries, and white granites of the western dome of the Arga-Ynnykh-Khaya Massif (Yakutiya) have been studied with emphasis on the white granites. The main features of its magmatic crystallization and initial transformation have been obtained by investigating the intensity of transformations using stochastic Markov models. The most widespread transformation is albitization. Two varieties exist. First, and most common, is development of a secondary albite crystal between two primary grains of potassium feldspar. Second, secondary albite has developed between primary quartz grains. Both variants have definite probabilities of occurrence. Less commonly, but with a constant probability, a secondary quartz grain forms as an intergrowth between two grains of potassium feldspar.