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

R.T. Pidgeon, M.J.B. Macambira, J.-M. Lafon

Open source

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

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