Neodymium isotope systematics of the mantle beneath the Baltic shield: Evidence for depleted mantle evolution since the Archaean-Reference-Cited by-同舟云学术

Neodymium isotope systematics of the mantle beneath the Baltic shield: Evidence for depleted mantle evolution since the Archaean

Published:1995-06 Issue:3-4 Volume:35 Page:235-243
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Andersen T.,Sundvoll B.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference62 articles.

1. Age, tectonic setting and provenance of Østfold-Marstrand Belt supracrustals: Westward crustal growth of the Baltic Shield at 1760 Ma;Åhäll;Precambrian Res.,1989

2. Mantle and crustal components in a carbonatite complex, and the evolution of carbonatite magma: REE and isotopic evidence from the Fen complex S.E. Norway;Andersen;Chem. Geol. (Isotope Geoscience Section),1987

3. Strontium and neodymium isotopic composition of an early tinguaite (nepheline microsyenite) in the Fen complex S.E. Norway: Age and petrogenetic implications;Andersen;Nor. Geol. Unders. Bull.,1986

4. Lead isotope geochemistry of the Fen carbonatite complex S.E. Norway: Age and petrogenetic implications;Andersen;Geochim. Cosmochim. Acta,1988

5. Sr, Nd and Pb isotopic characteristics of the Alnö carbonatite complex;Andersen,1995

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