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Trace element and Sr-Nd isotopic constraints on the compositions of lithospheric primary sources of Serra Geral continental flood basalts, southern Brazil

Hughes, S. S. and Schmitt, R. A. and Wang, Y. L. and Wasserburg, G. J. (1986) Trace element and Sr-Nd isotopic constraints on the compositions of lithospheric primary sources of Serra Geral continental flood basalts, southern Brazil. Geochemical Journal, 20 (4). pp. 173-189. ISSN 0016-7002. https://resolver.caltech.edu/CaltechAUTHORS:20131022-111252758

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Abstract

Multi-element abundances in twenty-four samples from the Serra Geral continental flood basalt system (Parana Basin) were determined by INAA to assess the trace element signature of primary magmatric sources. Isotopic Sr and Nd data were obtained on a 24-sample composite and three individual samples of the suite to constrain the influences of older enriched material. Twenty basaltic samples have enriched LILE commensurate with most continental tholeiites and, display fractionated REE patterns similar to those in the Columbia River Group and other flood basalt provinces. The mafic units exhibit low-moderate Ti, variable V, Cr and Ni and relatively uniform Co and Sc abundances. Four intermediate to silicic units exhibit higher overall incompatible element abundances, strongly fractionated patterns and depletions of compatible elements consistent with derivation by fractionation of basaltic parents. Isotopic data for two basalts and the composite analysis indicate ^(87)Sr/^(86)Sr = 0.7090 to 0.7105 and εNd = -6.6 to -6.9 requiring magma genesis in an evolved LILE-enriched upper mantle or lower crust. A silicic sample has ^(87)Sr/^(86)Sr = 0.7219 and εNd = -9.2 reflecting a stronger crustal influence. Chemical comparisons within the basaltic members allow the delineation of ten least-evolved compositions having a regionally characteristic trace element pattern and two additional samples (of one flow) representing a second, less fractionated pattern. Trace element models for both types predict magma segregation from lower lithospheric sources having relatively uniform enrichments of incompatible elements via regional metasomatism. The most viable scenarios for basalt magma production require either enriched mantle partial-melt liquids, some of which comingle with crustal components, or partial melting of ultramafic, LILE-enriched lower crust. Either process requires a zone of primary magma extraction in a region where initially uniform source enrichments act independently of subsequent contamination, probably in the crust/mantle transition zone.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.2343/geochemj.20.173DOIArticle
https://www.jstage.jst.go.jp/article/geochemj1966/20/4/20_4_173/_articlePublisherArticle
Additional Information:© 1986 Geochemical Society of Japan. Received December 12, 1985; Accepted April 23, 1986. We thank A. Roisenberg for providing the suite of Serra Geral samples and T. V. Anderson, W. T. Carpenter and D. Pratt for assistance with neutron activations in the Oregon State University TRIGA reactor. Helpful comments and criticisms by R. V. Fodor greatly improved the manuscript. Financial support was provided by NASA grant NAG9-63 to R. A. Schmitt and grant NAG9-49 to G. J. Wasserburg.
Funders:
Funding AgencyGrant Number
NASANAG9-63
NASANAG9-49
Issue or Number:4
Record Number:CaltechAUTHORS:20131022-111252758
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20131022-111252758
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42007
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:24 Oct 2013 23:55
Last Modified:03 Oct 2019 05:54

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