Th–U–Pb isotopic systems and internal structures of complex zircons from an enderbite from the Pium Complex, Carajás Province, Brazil: evidence for the ages of granulite facies metamorphism and the protolith of the enderbite
- DOI
- 10.1016/s0009-2541(99)00190-4
- Published
- 2000-05
- Container
- Chemical Geology
- Publisher
- Elsevier BV
- Open access
- unknown
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BibTeX
@article{allodium:10.1016/s0009-2541-99-00190-4,
title = {Th–U–Pb isotopic systems and internal structures of complex zircons from an enderbite from the Pium Complex, Carajás Province, Brazil: evidence for the ages of granulite facies metamorphism and the protolith of the enderbite},
author = {R.T. Pidgeon and M.J.B. Macambira and J.-M. Lafon},
year = {2000},
journal = {Chemical Geology},
doi = {10.1016/s0009-2541(99)00190-4},
url = {https://doi.org/10.1016/s0009-2541(99)00190-4}
}RIS
TY - JOUR TI - Th–U–Pb isotopic systems and internal structures of complex zircons from an enderbite from the Pium Complex, Carajás Province, Brazil: evidence for the ages of granulite facies metamorphism and the protolith of the enderbite AU - R.T. Pidgeon AU - M.J.B. Macambira AU - J.-M. Lafon PY - 2000 JO - Chemical Geology DO - 10.1016/s0009-2541(99)00190-4 UR - https://doi.org/10.1016/s0009-2541(99)00190-4 ER -
APA
Pidgeon, R., Macambira, M., & Lafon, J. (2000). Th–U–Pb isotopic systems and internal structures of complex zircons from an enderbite from the Pium Complex, Carajás Province, Brazil: evidence for the ages of granulite facies metamorphism and the protolith of the enderbite. Chemical Geology. https://doi.org/10.1016/s0009-2541(99)00190-4
Source records
- crossref · retrieved 2026-09-26T07:44:48.711Z