Zircon U-Pb geochronology and emplacement history of intrusive rocks in the Ardestan section, central Iran

Zircon U-Pb geochronology and emplacement history of intrusive rocks in the Ardestan section, central Iran

The Urumieh-Dokhtar Magmatic Arc (UDMA) is part of the Alpine–Himalayan orogenic belt and interpreted to be a subduction-related Andean-type magmatic arc. Along this belt, Eocene volcanics and some gabbroic to granitic bodies crop out. The main rock types of the studied intrusion are granite, grano...

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Bibliographic Details
Main Authors: F. SARJOUGHIAN, A. KANANIAN
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2017-02-01
Series:Geologica Acta
Subjects:
Zircon
Geochronology
Ardestan
Urumieh-Dokhtar Magmatic Arc belt
Iran
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/14461

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https://revistes.ub.edu/index.php/GEOACTA/article/view/14461

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