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-List Of Titles -Hf-Nd isotope and trace element constraints on subduction inputs at island arcs : limitations of Hf anomalies as sediment input indicators

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/139585

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Title
Hf-Nd isotope and trace element constraints on subduction inputs at island arcs : limitations of Hf anomalies as sediment input indicators
Related
Earth and planetary science letters, Vol. 304, Issue 1-2, (2011), p.212-223
DOI
10.1016/j.epsl.2011.01.034
Publisher
Elsevier BV
Date
2011
Author/Creator
Handley, Heather K
Author/Creator
Turner, Simon
Author/Creator
Macpherson, Colin G
Author/Creator
Gertisser, Ralf
Author/Creator
Davidson, Jon P
Description
New Nd-Hf isotope and trace element data for Javanese volcanoes are combined with recently published data to place constraints on subduction inputs at the Sunda arc in Indonesia and assess the value of Hf anomalies (expressed as Hf/Hf* and Sm/Hf ratios) as tracers of such inputs. Hf anomaly does not correlate with Hf isotope ratio in Javanese lavas, however, Hf/Hf* and Sm/Hf ratios do correlate with SiO2. Contrary to previous work, we show that Hf anomaly variation may be controlled by fractionation of clinopyroxene and/or amphibole during magmatic differentiation and does not represent the magnitude or type of subduction input in some arcs. Correlation of Sm/Hf with indices of differentiation for other arcs (e.g., Vanuatu, New Britain, and Mariana) suggests that differentiation control on Sm/Hf ratios in volcanic arc rocks may be a relatively common phenomenon. This study corroborates the use of Nd-Hf isotope co-variations in arc volcanic rocks to ascertain subduction input characteristics. The trajectories of regional volcano groups (East, Central and West Java) in Nd-Hf isotope space reveal heterogeneity in the subducted sediment input along Java, which reflects present-day spatial variations in sediment compositions on the down-going plate in the Java Trench. The high Sm/Hf ratio required in the sediment end-member for some Javanese basalts suggests that partial melting of subducted sediment occurs in the presence of residual zircon, and is inconsistent with residual monazite or allanite.
Description
12 page(s)
Subject Keyword
Hf anomaly
Subject Keyword
Magma genesis
Subject Keyword
Nd-Hf isotopes
Subject Keyword
Sediment subduction
Subject Keyword
Sm/Hf
Subject Keyword
Sunda arc
Resource Type
journal article
Organisation
Macquarie University. Dept. of Earth and Planetary Sciences

Identifier
http://hdl.handle.net/1959.14/139585
Identifier
ISSN:0012-821X
Identifier
mq_res-ext-2-s2.0-79952626932
Language
eng
Reviewed
Reviewed
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Citation Format
E-mail Address
Subject
"Earth and planetary science letters"
 
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