Oxygen isotope compositions and magmatic epidote from two contrasting metaluminous granitoids, NE Brazil View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2003-05

AUTHORS

V. P. Ferreira, J. W. Valley, A. N. Sial, M. J. Spicuzza

ABSTRACT

Oxygen isotope compositions of mineral separates were determined from two metaluminous granitoids (Emas and São Rafael plutons) from northeastern Brazil. The I-type Emas pluton has high δ18O (WR) values (11.5–11.8‰), whereas the São Rafael pluton has low δ18O (WR) values (7.5–8.1‰), but Sr and Nd are characteristics of S-type granitoids. Measured mineral–mineral fractionations suggest continuous sub-solidus inter-mineral isotope exchange among all minerals except zircon. There is a large and consistent quartz–epidote fractionation that gives apparent temperatures that are much lower than anticipated closure temperatures for epidote. Oxygen isotope fractionation between natural zircon and magmatic epidote is opposite to that predicted from theoretical determinations, as δ18O (epidote) <δ18O (zircon). An empirical calibration based on these results would suggests a closure T for oxygen in epidote of ~500 °C and Δ(qtz–epi) ~5.19 at 500 °C. More... »

PAGES

205-216

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s00410-003-0443-4

DOI

http://dx.doi.org/10.1007/s00410-003-0443-4

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1013700999


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