In hypersolvus granites, as used by Tuttle and Bowen in 1958, crystallization at relatively low water pressures results in the formation of a single feldspar as opposed to subsolvus granites in which two distinct types of feldspar are present. The distinctive character of feldspar in hypersolvus granite is to present exsolution textures.
In hypersolvus granites, as used by Tuttle and Bowen in 1958, crystallization at relatively low water pressures results in the formation of a single feldspar as opposed to subsolvus granites in which two distinct types of feldspar are present. The distinctive character of feldspar in hypersolvus granite is to present exsolution textures.
Source: Wikipedia "Hypersolvus" · CC BY-SA 4.0
Share this article: X · Bluesky