High degree partial melting of the metasomatized mantle: A possible source for the Eocene-Oligocene porphyry Cu-Au-Mo deposits in Lut block, Eastern Iran-Reference-Cited by-同舟云学术

High degree partial melting of the metasomatized mantle: A possible source for the Eocene-Oligocene porphyry Cu-Au-Mo deposits in Lut block, Eastern Iran

Published:2023-06 Issue: Volume:157 Page:105386
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Almasi Alireza^ORCID,Nabatian Ghasem,Mahdavi Amir^ORCID,Li Qiuli

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference180 articles.

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4. Temporal–spatial distribution and tectonic setting of porphyry copper deposits in Iran: Constraints from zircon U-Pb and molybdenite Re–Os geochronology;Aghazadeh;Ore Geol. Rev.,2015

5. High magmatic flux during Alpine-Himalayan collision: Constraints from the Kal-e-Kafi complex, central Iran;Ahmadian;Geol. Soc. Am. Bull.,2009

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