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Autor:
Afsaneh Soltani, Alireza Zarasvandi, Nader Taghipour, Mohsen Rezaei, Adel Saki, Morteza Sajjadiyan, Ghazal Zarasvandi
Publikováno v:
Journal of Economic Geology, Vol 16, Iss 2, Pp 163-206 (2024)
The Kuh-e-Esfand copper deposit is located in the southernmost part of the Urmia-Dokhtar magmatic belt. The Oligocene-Miocene intrusive bodies, ranging from diorite to quartz diorite and granodiorite, are emplaced within the Eocene volcanic complex.
Externí odkaz:
https://doaj.org/article/0454742188dc4bad94746342b20d1585