Ar-40/Ar-39 geochronology of magmatic and metasomatic events in the Sora porphyry Cu-Mo ore cluster (Kuznetsk Alatau)

Citation
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
Citations number
59
Categorie Soggetti
Earth Sciences
Journal title
GEOLOGIYA I GEOFIZIKA
ISSN journal
00167886 → ACNP
Volume
42
Issue
5
Year of publication
2001
Pages
786 - 801
Database
ISI
SICI code
0016-7886(2001)42:5<786:AGOMAM>2.0.ZU;2-Z
Abstract
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.