Extreme enrichment of high field strength elements in Jericho eclogite xenoliths: A cryptic record of Paleoproterozoic subduction, partial melting, and metasomatism beneath the Slave craton, Canada-Reference-Cited by-同舟云学术

Extreme enrichment of high field strength elements in Jericho eclogite xenoliths: A cryptic record of Paleoproterozoic subduction, partial melting, and metasomatism beneath the Slave craton, Canada

Published:2002 Issue:6 Volume:30 Page:507
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:Geol

Author:

Heaman Larry M.,Creaser Robert A.,Cookenboo Harrison O.

Publisher

Geological Society of America

Subject

Geology

Reference19 articles.

1. Geochemistry of xenolithic eclogites from West Africa, part I: A link between low MgO eclogites and archean crust formation

2. Anisotropic upper-mantle stratigraphy and architecture of the Slave craton

3. Rutile-aqueous fluid partitioning of Nb, Ta, Hf, Zr, U and Th: implications for high field strength element depletions in island-arc basalts

4. Frozen subduction in Canada's Northwest Territories: Lithoprobe deep lithospheric reflection profiling of the western Canadian Shield

5. U-Pb zircon and rutile ages from granulite xenoliths in the Slave province: Evidence for mafic magmatism in the lower crust coincident with Proterozoic dike swarms

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