Geochemistry and petrogenesis of mafic and intermediate dyke swarms in eastern Tafresh (Urumieh-Dokhtar magmatic belt)
IntroductionThe Urumieh-Dokhtar magmatic belt is one of the most active magmatic regions of Iran during the Cenozoic era. There are differing views regarding the tectonomagmatic setting of this magmatism; some attribute it to active continental margin magmatism, island arcs, post-collisional regions...
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| Main Authors: | , |
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| Format: | Article |
| Language: | fas |
| Published: |
University of Isfahan
2025-05-01
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| Series: | پترولوژی |
| Subjects: | |
| Online Access: | https://ijp.ui.ac.ir/article_29271_d4393d704cbf206b5676d5aada13fbab.pdf |
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