Zircon U--Pb ages of Au-bearing host rocks in Northwest Iran as evidence for gold mineralization in the Carboniferous, not Cenozoic time!-Reference-Cited by-同舟云学术

Zircon U--Pb ages of Au-bearing host rocks in Northwest Iran as evidence for gold mineralization in the Carboniferous, not Cenozoic time!

Published:2021-03 Issue: Volume:384-385 Page:105974
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Daneshvar Narges,Maanijou Mohammad,Azizi Hossein,Lentz David R.,McFarlane Chris R.M.

Funder

Universidade de Brasília

Bu-Ali Sina University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference74 articles.

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3. Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution;Alavi;Am. J. Sci.,2004

4. Geochemistry and zircon geochronology of the Permian A-type Hasanrobat Granite, Sanandaj–Sirjan belt: a new record of the Gondwana break-up in Iran;Alirezaei;Lithos,2012

5. Orogenic gold mineralization in the Qolqoleh deposit, Northwestern Iran;Aliyari;Resour. Geol.,2007

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1. Geochemistry and origin of the Late Carboniferous ultramafic, mafic, and felsic plutonic rocks (NW Iran);Lithos;2024-09

2. From Early Jurassic intracontinental subduction to Early-Middle Jurassic slab break-off magmatism during the Cimmerian orogeny in the Sanandaj-Sirjan Zone, Iran;Journal of Asian Earth Sciences;2024-05