西藏花岗岩类中长石的特征与花岗岩类的演化

THE CHARACTERISTICS OF FELDSPARS IN GRANITOIDS AND THE EVOLUTION OF XIZANG GRANITES

The coefficient (K) and distribution frequency of alkali feldspars in Xizang granitoids arc higher in later stages as compared with those in earlier stages The An value of plagioclase gradually decreases from earlier to later Stages. The Ab value of alkali feldspars of earlier stages is lower than that of later stages. Alkali feldspars from ordered to disordered have been all discovered. For most plutons, the extent of orer-disorder between alkali feldspar phenocrysts and groundmass is basically similar. On the other hand, however, the majority of plagioclase is of ordered type. Feldspars of late Yenshanian are of higher order state than that of Himalayan. In the light of composition and structure state as mentioned above it can be said that granitoids in Southern Xizang have a magmatie origin and they tend to be more acidic during their evolution from earlier to later stages.

The coefficient (K) and distribution frequency of alkali feldspars in Xizang grani-toids are higher in later stages as compared with those in earlier stages. The An value of plagioclase gradually decreases from earlier to later stages. The Ab value of alkali feld-spars of earlier stages is lower than that of later stages.Alkali feldspars from ordered to disordered have been all discovered. For most plu-tons, the extent of orer-disorder between alkali feldspar phenoerysts and groundmass is basically similar. On the other hand, however, the majority of plagioclase is of ordered type. Feldspars of late Yenshanian are of higher order state than that of Himalayan.In the light of composition and structure state as mentioned above it can be said that granitoids in Southern Xizang have a magmatic origin and they tend to be more acidic during their evolution from earlier to later stages.