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Cited by 401

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Trace element evidence from seamounts for recycled oceanic crust in the Eastern Pacific mantle

NIU, Y, BATIZA, R·1997·Earth and Planetary Science Letters

Abstract

We present trace element data for 80 samples from about 50 seamounts in the east equatorial Pacific near the East Pacific . Rise. These data indicate that the heterogeneous mantle source that supplies the seamounts consists of two components: 1 . an extremely depleted component, much more depleted than estimates of the source of depleted MORB; and 2 an enriched component even more enriched than average OIB. The depleted component shows large variations in ZrrHf, NbrTa, RbrCs, CerPb, and ThrU that are correlated with each other and with LarSm, indicating that these paired elements do fractionate from each other in some oceanic basalts. The order of incompatibility of trace elements we find differs slightly from that found elsewhere. For example, for seamounts, we find that D f D - D f D. In comparison with Th and U, Nb Th Ta U the enriched component shows anomalous enrichments of Ta and Nb. Since such fractionations are characteristic of subduction zones, we suggest that the most likely ultimate source of the enriched component is recycled ocean crust.

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Metadata

Authors
NIU, Y., & BATIZA, R.
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
1997-05
Volume
148
Issue
3-4
Pages
471-483
ISSN
0012-821X (ISSN-L)
OpenAlex
W2164064321
Cited by
401
References
28
FWCI
12.80
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Trace element evidence from seamounts for recycled oceanic crust in the Eastern Pacific mantle. https://app.cochat.ai/papers/10.1016/s0012-821x(97)00048-4
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NIU, Y., & BATIZA, R. (1997). Trace element evidence from seamounts for recycled oceanic crust in the Eastern Pacific mantle. Earth and Planetary Science Letters. https://doi.org/10.1016/s0012-821x(97)00048-4

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