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 gr...
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| Yayımlandı: | Geologica Acta: an international earth science journal |
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| Asıl Yazarlar: | , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Universitat de Barcelona
2017
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| Konular: | |
| Online Erişim: | https://www.redalyc.org/articulo.oa?id=50549984003 https://www.redalyc.org/journal/505/50549984003/ https://www.redalyc.org/journal/505/50549984003/html/ https://www.redalyc.org/journal/505/50549984003/50549984003.epub https://www.redalyc.org/journal/505/50549984003/movil |
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