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...
Salvato in:
| Autori principali: | , , , |
|---|---|
| Natura: | Artigo |
| Lingua: | Persa |
| Pubblicazione: |
University of Isfahan
2026-03-01
|
| Serie: | پترولوژی |
| Soggetti: | |
| Accesso online: | https://ijp.ui.ac.ir/article_30317_20c70b4d08ef46667d6468b0cc8bbc41.pdf |
| Tags: |
Nessun Tag, puoi essere il primo ad aggiungerne!!
|