A Preliminary Study on the Aghbolaq (Fe, Cu) Skarn Deposit, Oshnavieh, NW Iran: Constraints on Metasomatic Fluid Evolution
Author:
Affiliation:
1. Department of Earth Sciences University of Tabriz Tabriz 5166616471 Iran
2. Geology Department, Faculty of Sciences Urmia University Urmia 57153 Iran
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14689
Reference51 articles.
1. Zagros orogeny: a subduction-dominated process
2. The gabbro (shoshonitic)–monzonite–granodiorite association of Khankandi pluton, Alborz Mountains, NW Iran
3. Tectonics of the zagros orogenic belt of iran: new data and interpretations
4. Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution
5. Mineralogy, geochemistry, and evolution of the Mivehrood skarn and the associated pluton, northwest Iran;Alirezaei S.;International Journal of Earth Sciences,2015
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1. Magmatic‐hydrothermal evolution and mineralization mechanisms of the Wangjiazhuang Cu (‐Mo) Deposit in Zouping Volcanic Basin, Shandong Province, China: Constraints from Fluid Inclusions;Acta Geologica Sinica - English Edition;2023-12-09
2. The Characteristics and Origin of Barite in the Giant Mehdiabad Zn-Pb-Ba Deposit, Iran;Economic Geology;2023-09-01
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