Magnetite chemistry in the Dalli porphyry Cu-Au deposit, central Urumieh-Dokhtar Magmatic Arc (UDMA)

The Dalli porphyry Cu-Au deposit is located in the central parts of Urumieh –Dokhtar Magmatic Arc (UDMA). This deposit is formed via the emplacing of Miocene intrusions mainly containing diorite and quartz diorite within the Eocene andesite and porphyritic basaltic andesite units. Main alterations i...

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Bibliographic Details
Published inJournal of Economic Geology Vol. 15; no. 1; pp. 1 - 25
Main Authors Alireza Zarasvandi, Mohsen Rezaei, Shima Azizi, Mansour Adelpour, Adel Saki
Format Journal Article
LanguageEnglish
Persian
Published Ferdowsi University of Mashhad 01.05.2023
Subjects
dalli porphyry
hydrothermal evolution
magnetite chemistry
urumieh-dokhtar magmatic arc (udma)
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