Genetic comparison of lead-zinc deposits of central Taurus.

dc.contributor.authorAyhan A.
dc.date.accessioned2020-03-26T16:10:03Z
dc.date.available2020-03-26T16:10:03Z
dc.date.issued1984
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractSeveral carbonate-bearing and sulphide lead-zinc deposits in Central Taurus, which are deposited generally in carbonate rocks of different tectonic units by different mechanisms, can be divided into 6 groups these are listed and described. All geological data show that the ore deposits are not deposited by a single geological process at a definite time interval. All deposits include karstification products, according to paleoclimatic processes and their paleogeographic positions especially in Paleocene.-from Authoren_US
dc.identifier.endpage342en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage335en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/16056
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherMineral Research & Exploration Institute (MTA), Ankaraen_US
dc.relation.ispartofGeology of the Taurus Belt. International symposium, 1983, Ankaraen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.titleGenetic comparison of lead-zinc deposits of central Taurus.en_US
dc.typeArticleen_US

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