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Types of massive sulphide deposits in the Urals

Mineralium Deposita : Volume 33

Mineralium Deposita : Volume 32

Types of massive sulphide deposits in the Urals

Content Provider	Springer Nature Link
Author	Prokin, V. A. Buslaev, F. P. Nasedkin, A. P.
Copyright Year	1998
Abstract	Massive sulphide deposits in the Urals are found within volcanic and volcanic-sedimentary sequences of Ordovician to Middle Devonian ages. Four types of economic sulphide deposits have been recognized: Cyprus, Besshi, Urals and Baimak. The Cyprus-type copper sulphide deposits are hosted by mafic volcanites that occur in the basal parts of Palaeozoic volcanic sequences. The Besshi-type copper-zinc deposits are located within clastic sedimentary rocks intercalated with basalts and andesites. Zinc-copper deposits of the Urals-type are hosted by bimodal rhyolite-basalt assemblages, which occur at a higher stratigraphic level than those of Cyprus- and Besshi-types. The Baimak-type zinc-copper-barite deposits are associated with intrusive quartz porphyries which occur in the upper parts of bimodal volcanic successions. In addition there are some sulphide deposits of zinc-lead-barite and zinc-copper composition hosted by Ordovician terrigenous sequences which occur within depressions in Precambrian blocks. These types of sulphide deposits have been formed at various stages of divergence and convergence of the Earth's crust during the orogenic history of the Urals.
Starting Page	121
Ending Page	126
Page Count	6
File Format	PDF
ISSN	00264598
Journal	Mineralium Deposita
Volume Number	34
Issue Number	1
e-ISSN	14321866
Language	English
Publisher	Springer-Verlag
Publisher Date	1998-11-19
Publisher Place	Berlin/Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Content Type	Text
Resource Type	Article
Subject	Geophysics Economic Geology Geochemistry and Petrology

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