Surface layer Nd isotopic composition of ferromanganese crusts collected from the Takuyo-Daigo Seamount reflects ambient seawater
Author:
Affiliation:
1. Project Team for Development of New-generation Research Protocol for Submarine Resources, Japan Agency for Marine-Earth Science Technology (JAMSTEC)
2. Department of Geology, Kochi University
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Link
https://www.jstage.jst.go.jp/article/geochemj/51/1/51_2.0463/_pdf
Reference20 articles.
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2. Amakawa, H., Sasaki, K. and Ebihara, M. (2009) Nd isotopic Surface layer Nd isotopic composition of Fe-Mn crusts collected from the Takuyo-Daigo Seamount e7 composition in the central North Pacific. Geochim. Cosmochim. Acta 73, 4705–4719.
3. Burton, K. W., Ling, H.-F. and O’Nions, R. K. (1997) Closure of the Central American Isthmus and its effect on deep-water formation in the North Atlantic. Nature 386, 382–385.
4. Foster, G. L. and Vance, D. (2006) In situ Nd isotopic analysis of geological materials by laser ablation MC-ICP-MS. J. Anal. At. Spectrom. 21, 288–296.
5. Frank, M. (2002) Radiogenic isotopes: tracers of past ocean circulation and erosional input. Rev. Geophys. 40, 1001 (http://dx.doi.org/10.1029/2000RG000094).
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