Abstract
Diorites are mainly of two types—hornblende diorites and biotite diorites having transitions between them. The former possesses panidiomorphic and the latter allotrimorphic texture. Hornblende diorite is considered to be a magmatic rock and the biotite diorite is formed by assimilation of the hornblende diorite by granite magma.
Similar content being viewed by others
References
Thompson, J. B., Role of aluminium in rock-forming silicates,Geol. Soc. Amer. Bull. 58 1232 (1947).
Buerger, M. T., The role oI temperature in mineralogy,Amer. Min. 33 101 (1948).
Kushiro, I., Si-Al relation in clinopyroxenes from igneous rocks,Amer. J. Sci. 258 548–554 (1960).
Sundius, N., The classification of the hornblendes and the solid solution relations in the amphibole groups, Sveriges,Geol. Undersokning Ser. Arsbok 40 1–31 (1946).
Gulson, B. L., Lovering, J. R., Taylor, S. R. and White, A. J. R., High Kdiorites, their place in the calcalkaline association and relationship to andesites,Lithos 5 269–279 (1972).
Nockolds, S. R., The contaminated granite of Bibette head, Aldarmey,Geol. Mag. 69 433–452 (1932).
Thomas, H. H. and Bailey, E. B., Tertiary and Post-Tertiary Geology of Mull, Lock Aline and Oban,Mem. Geol. Surv. U.K. (1924).
Nockolds, S. R., Some theoretical aspects of contamination of acid magmas,Jour. Geol. 41 561–589 (1933).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Reddy, G.L., Murty, M.S. Diorites from Kuderu and Atmakuru areas, Anantapur District, Andhra Pradesh. Proc. Indian Acad. Sci. 82, 155–166 (1975). https://doi.org/10.1007/BF03050529
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF03050529