U-Pb (SHRIMP) geochronology of pre-hercynian granitoids of the Iberian Variscan fold belt (northern central Portugal): evidence for a Cadomian magmatic event (1999)
- Authors:
- Autor USP: CORDANI, UMBERTO GIUSEPPE - IGC
- Unidade: IGC
- Assunto: GEOCRONOLOGIA
- Language: Inglês
- Imprenta:
- Publisher: Cambridge Publications
- Publisher place: Strasbourg
- Date published: 1999
- Source:
- Título do periódico: Journal of Conference Abstracts.
- Conference titles: European Union of Geosciences Conference
-
ABNT
VALLE, Beatriz e CORDANI, Umberto G. U-Pb (SHRIMP) geochronology of pre-hercynian granitoids of the Iberian Variscan fold belt (northern central Portugal): evidence for a Cadomian magmatic event. 1999, Anais.. Strasbourg: Cambridge Publications, 1999. Disponível em: https://repositorio.usp.br/directbitstream/ec4ce4ea-c305-497a-8d51-c8cb09433ec5/1482754.pdf. Acesso em: 19 jul. 2024. -
APA
Valle, B., & Cordani, U. G. (1999). U-Pb (SHRIMP) geochronology of pre-hercynian granitoids of the Iberian Variscan fold belt (northern central Portugal): evidence for a Cadomian magmatic event. In Journal of Conference Abstracts.. Strasbourg: Cambridge Publications. Recuperado de https://repositorio.usp.br/directbitstream/ec4ce4ea-c305-497a-8d51-c8cb09433ec5/1482754.pdf -
NLM
Valle B, Cordani UG. U-Pb (SHRIMP) geochronology of pre-hercynian granitoids of the Iberian Variscan fold belt (northern central Portugal): evidence for a Cadomian magmatic event [Internet]. Journal of Conference Abstracts. 1999 ;[citado 2024 jul. 19 ] Available from: https://repositorio.usp.br/directbitstream/ec4ce4ea-c305-497a-8d51-c8cb09433ec5/1482754.pdf -
Vancouver
Valle B, Cordani UG. U-Pb (SHRIMP) geochronology of pre-hercynian granitoids of the Iberian Variscan fold belt (northern central Portugal): evidence for a Cadomian magmatic event [Internet]. Journal of Conference Abstracts. 1999 ;[citado 2024 jul. 19 ] Available from: https://repositorio.usp.br/directbitstream/ec4ce4ea-c305-497a-8d51-c8cb09433ec5/1482754.pdf - Precambrian cratonic areas, mobile belts and sedimentary covers
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