A trace element study of siderite–jasper banded iron formation in the 3.45Ga Warrawoona Group, Pilbara Craton—Formation from hydrothermal fluids and shallow seawater-Reference-Cited by-同舟云学术

A trace element study of siderite–jasper banded iron formation in the 3.45Ga Warrawoona Group, Pilbara Craton—Formation from hydrothermal fluids and shallow seawater

Published:2005-04 Issue:1-2 Volume:137 Page:93-114
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Bolhar Robert,Van Kranendonk Martin J.,Kamber Balz S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference49 articles.

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3. Effects on syn- and post-depositional processes on rare-earth element distribution in Precambrian iron formations;Bau;Eur. J. Mineral.,1993

4. Distribution of Y and rare-earth elements in the Penge and Kuruman Iron Formations, Traansvaal Supergroup, South Africa;Bau;Precambr. Res.,1996

5. Comparing yttrium and rare earths in hydrothermal fluids from the Mid-Atlantic Ridge: implications for Y and REE behaviour during near-vent mixing and for the Y/Ho ratio of Proterozoic seawater;Bau;Chem. Geol.,1999

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