The data which I obtained: a mantle ratio of 87Sr/86Sr; and 34S/32S of sulphides

calc-alkaline; granodiorite, quartz monzonite composition of host porphyry granitoids; I type chemistry; within plate granite; good development of hydrothermal alteration zonation of central potassic alteration to the phyllic and argillic alteration etc. Its host rock possess an extremely low value of copper (< 1.0 ppm) and quartz enclaves/ chilling quartz with the sulphide cummulates etc. I am in favour of accepting this occurrence as a potential for porphyry type mineralization. Please suggest if it is truely an occurrence of economic worth and under such condition Magma Mixing Model is a valid proposition or not?

More Dilip Majumdar's questions See All
Similar questions and discussions