Oxygen isotope systematics of the Banda Arc: low δ18O despite involvement of subducted continental material in magma genesis

P. Z. Vroon; D. Lowry; M. J. Van Bergen; A. J. Boyce; D. P. Mattey

doi:10.1016/S0016-7037(00)00554-8

Oxygen isotope systematics of the Banda Arc: low δ¹⁸O despite involvement of subducted continental material in magma genesis

P. Z. Vroon, D. Lowry, M. J. Van Bergen, A. J. Boyce, D. P. Mattey

Department of Earth Sciences

Research output: Contribution to journal › Article › peer-review

Original language	English
Pages (from-to)	589-609
Number of pages	21
Journal	Geochimica et Cosmochimica Acta
Volume	65
Issue number	4
Early online date	13 Feb 2001
DOIs	https://doi.org/10.1016/S0016-7037(00)00554-8
Publication status	Published - 15 Feb 2001

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10.1016/S0016-7037(00)00554-8

Cite this

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title = "Oxygen isotope systematics of the Banda Arc: low δ18O despite involvement of subducted continental material in magma genesis",

author = "Vroon, {P. Z.} and D. Lowry and {Van Bergen}, {M. J.} and Boyce, {A. J.} and Mattey, {D. P.}",

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AU - Boyce, A. J.

AU - Mattey, D. P.

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Oxygen isotope systematics of the Banda Arc: low δ18O despite involvement of subducted continental material in magma genesis

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Oxygen isotope systematics of the Banda Arc: low δ¹⁸O despite involvement of subducted continental material in magma genesis