Vi. Sotnikov et al., Ar-40/Ar-39 geochronology of magmatic and metasomatic events in the Sora porphyry Cu-Mo ore cluster (Kuznetsk Alatau), GEOL GEOFIZ, 42(5), 2001, pp. 786-801
Ar-40/Ar-39 dating (23 determinations) has been carried out for magmatic an
d ore-metasomatic processes in the Sera copper-molybdenum ore region. Forma
tion of the large Sera porphyry Cu-Mo deposit related to the evolution of a
n ore-bearing porphyry complex was preceded by long formation of multipulse
granitoid magmatism, separate pulses of which were accompanied by the occu
rrence of Cu-Mo-skarn mineralization and K-feldspathic metasomatites with d
ispersed chalcopyrite and molybdenite. The total age range of endogenic eve
nts in the regions is 481-356 Ma. The evolution of the ore-bearing porphyry
complex and related ore-metasomatic processes proceeded in several stages.
The major industrial porphyry Cu-Mo mineralization of the Sera deposit is
related to the first porphyry stage (389-388 Ma BP). The occurrence of ore-
bearing porphyries and ore-metasomatic formations was preceded by intrusion
of pre-ore dikes (405-402 Ma BP). The same geochemical profile (Cu, Mo) of
ore mineralizations formed at different stages of multipulse magmatism and
the similar petrogeochemical compositions and low (Sr-87/Sr-86)(0) values
of magmatites evidence their genesis in the same zone of magma formation.