Magnetite chemistry of the Sarkuh Porphyry Cu deposit, Urumieh–Dokhtar Magmatic Arc (UDMA), Iran: A record of deviation from the path sulfide mineralization in the porphyry copper systems-Reference-Cited by-同舟云学术

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Magnetite chemistry of the Sarkuh Porphyry Cu deposit, Urumieh–Dokhtar Magmatic Arc (UDMA), Iran: A record of deviation from the path sulfide mineralization in the porphyry copper systems

Published:2023-06 Issue: Volume:249 Page:107213
ISSN:0375-6742
Container-title:Journal of Geochemical Exploration
language:en
Short-container-title:Journal of Geochemical Exploration

Author:

Zarasvandi Alireza,Rezaei Mohsen,Raith Johann G.,Taheri Milad,Asadi Sina,Heidari Majid

Funder

Shahid Chamran University of Ahvaz

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology

Reference70 articles.

1. Structures of the Zagros fold-thrust belt in Iran;Alavi;Am. J. Sci.,2007

2. Triggers for the generation of post-collisional porphyry Cu systems in the Kerman magmatic copper belt, Iran: new constraints from elemental and isotopic (Sr–Nd–Hf–O) data;Asadi;Gondwana Res.,2018

3. Discriminating productive and barren porphyry copper deposits in the southeastern part of the central Iranian volcano-plutonic belt, Kerman region, Iran: a review;Asadi;Earth-Sci. Rev.,2014

4. Special Paper: the composition of magmatic-hydrothermal fluids in barren and mineralized intrusions;Audétat;Econ. Geol.,2008

5. The oxidation state of vanadium in titanomagnetite from layered basic intrusions;Balan;Am. Mineral.,2006

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