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Apatite U-Pb dating at UNAM laboratories: analytical protocols and examples of its application

Apatite is the most common phosphate mineral in the Earth’s crust and can be found in practically all magmatic and metamorphic rocks, as well as in ancient and recent sediments and in certain ore deposits. Its effective closure temperature of 450–550 °C for the U-Pb system makes apatite an important...

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Detalhes bibliográficos
Publicado no:Revista Mexicana de Ciencias Geológicas
Principais autores: Carlos Ortega-Obregón, Fanis Abdullin, Luigi Solari, Peter Schaaf, Gabriela Solís-Pichardo
Formato: Artigo
Idioma:Inglês
Publicado em: Universidad Nacional Autónoma de México 2019
Assuntos:
Acesso em linha:https://www.redalyc.org/articulo.oa?id=57265242003
https://www.redalyc.org/journal/572/57265242003/
https://www.redalyc.org/journal/572/57265242003/html/
https://www.redalyc.org/journal/572/57265242003/57265242003.epub
https://www.redalyc.org/journal/572/57265242003/movil
https://doi.org/10.22201/cgeo.20072902e.2019.1.749
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