Neodymium isotopic study of rare earth element sources and mobility in hydrothermal Fe oxide (Fe-P-REE) systems-Reference-Cited by-同舟云学术

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Neodymium isotopic study of rare earth element sources and mobility in hydrothermal Fe oxide (Fe-P-REE) systems

Published:2000-03 Issue:6 Volume:64 Page:1059-1068
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Gleason James D.,Marikos Mark A.,Barton Mark D.,Johnson David A.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference46 articles.

1. Anderson R. E. (1970) Ash-flow tuffs of Precambrian age in southeast Missouri. Missouri Geol. Surv. & Water Res., Rept. Inv. 46.

2. An evaporitic-source model for igneous-related Fe-oxide-(REE-Cu-Au-U) mineralization;Barton;Geology,1996

3. A comparison of Fe-oxide (-Cu-Au-REE-U-Co-Ag) mineralization;Barton;Geol. Soc. Am. Abstr. Progr.,1997

4. Mesozoic contact metamorphism in the western United States;Barton,1988

5. A comparison of felsic and mafic Fe-P(-REE-Cu) Deposits;Barton;Geol. Soc. Am. Abstr. Progr.,1993

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