Geology, geochemistry, fluid inclusions, and H–O–C–S–Pb isotope constraints on the genesis of the Atash-Anbar epithermal gold deposit, Urumieh–Dokhtar magmatic arc, central-northern Iran

Author:

Tale Fazel Ebrahim,Nevolko Peter A.,Pašava Jan,Xie Yuling,Alaei Narges,Oroji Abbas

Funder

Česká geologická služba

Iranian Mines and Mining Industries Development and Renovation Organization

Siberian Branch, Russian Academy of Sciences

Bu-Ali Sina University

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference212 articles.

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2. Zagros orogeny: a subduction-dominated process;Agard;Geol. Mag.,2011

3. Aghanabati, A., 2004. Geology of Iran. Geol. Surv. Iran, Tehran, pp. 606 (in Persian).

4. Eocene K-rich adakitic rocks in the Central Iran: Implications for evaluating its Cu-Au-Mo metallogenic potential;Ahmadian;Ore Geol. Rev.,2016

5. Petrogenesis of Plio-Quaternary post-collisional ultrapotassic volcanism in NW of Marand, NW Iran;Ahmadzadeh;J. Asian Earth Sci.,2010

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