Geochemical evidence of dykes in the Salafchegan-Tafresh region as part of Cenozoic magmatism in the central segment of the Urumieh-Dokhtar magmatic arc
IntroductionIran constitutes a critical segment of the Alpine-Himalayan orogenic belt, formed through the collision of the Arabian, Indian and Eurasian tectonic plates (Rolland et al., 2002; Stampfli and Hochard, 2009; von Raumer et al., 2003; Yin and Harrison, 2000). The Urmia-Dokhtar magmatic arc...
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| Autors principals: | , , |
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| Format: | Artigo |
| Idioma: | Persa |
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University of Isfahan
2025-09-01
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| Col·lecció: | پترولوژی |
| Matèries: | |
| Accés en línia: | https://ijp.ui.ac.ir/article_29654_d0a32be979442585363eaabeedb6d625.pdf |
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