Detrital Zircon U–Pb Geochronology of the Muti Formation: Implications for Provenance and Evolution of the Oman Foreland Basin
Detrital zircon U–Pb dating from the Muti Formation sheds light on sediment sources and foreland basin development along the northeastern Arabian margin during the Late Cretaceous. The siliciclastic-rich Muti Formation was deposited in a syn-obduction foreland basin that formed as the Semail Ophioli...
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| Автори: | , , , , , |
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| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
MDPI AG
2025-12-01
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| Серія: | Geosciences |
| Предмети: | |
| Онлайн доступ: | https://www.mdpi.com/2076-3263/16/1/15 |
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