Diachronous Eocene-Oligocene granitoid magmatism in the southeastern part of the Urumieh-Dokhtar magmatic arc, Mardehak area, Jebal-e-Barez, Jiroft
IntroductionThe Zagros orogeny occurred through four main geodynamic events of the Wilson cycle, leading to the formation of the Neotethys oceanic basin: (i) intracontinental rifting in the Carboniferous, (ii) oceanic basin development in the Permian–Triassic, (iii) subduction of oceanic lithosphere...
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| Principais autores: | , , , |
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| Formato: | Artigo |
| Idioma: | Persa |
| Publicado em: |
University of Isfahan
2026-03-01
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| Colecção: | پترولوژی |
| Assuntos: | |
| Acesso em linha: | https://ijp.ui.ac.ir/article_30317_20c70b4d08ef46667d6468b0cc8bbc41.pdf |
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