Zircon trace element geochemistry: partitioning with garnet and the link between U–Pb ages and metamorphism

Daniela Rubatto

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DOI: 10.1016/s0009-2541(01)00355-2
Published: 2002-03
Container: Chemical Geology
Publisher: Elsevier BV
Open access: unknown

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Cite this work

BibTeX

@article{allodium:10.1016/s0009-2541-01-00355-2,
  title = {Zircon trace element geochemistry: partitioning with garnet and the link between U–Pb ages and metamorphism},
  author = {Daniela Rubatto},
  year = {2002},
  journal = {Chemical Geology},
  doi = {10.1016/s0009-2541(01)00355-2},
  url = {https://doi.org/10.1016/s0009-2541(01)00355-2}
}

RIS

TY  - JOUR
TI  - Zircon trace element geochemistry: partitioning with garnet and the link between U–Pb ages and metamorphism
AU  - Daniela Rubatto
PY  - 2002
JO  - Chemical Geology
DO  - 10.1016/s0009-2541(01)00355-2
UR  - https://doi.org/10.1016/s0009-2541(01)00355-2
ER  -

APA

Rubatto, D. (2002). Zircon trace element geochemistry: partitioning with garnet and the link between U–Pb ages and metamorphism. Chemical Geology. https://doi.org/10.1016/s0009-2541(01)00355-2

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crossref · retrieved 2026-09-26T22:59:48.720Z