Trace elements in olivine of ultramafic lamprophyres controlled by phlogopite-rich mineral assemblages in the mantle source-Reference-Cited by-同舟云学术

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Trace elements in olivine of ultramafic lamprophyres controlled by phlogopite-rich mineral assemblages in the mantle source

Published:2017-11 Issue: Volume:292-293 Page:81-95
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Veter Marina,Foley Stephen F.,Mertz-Kraus Regina,Groschopf Nora

Funder

Geocycles Research Centre of the University of Mainz

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference77 articles.

1. Low Ni in silica-understurated ultrapotassic igneous rocks as evidence for carbonate metasomatism in the mantle;Ammannati;Earth and Planetary Science Letters,2016

2. Olivine and the origin of kimberlite;Arndt;Journal of Petrology,2010

3. Mesoproterozoic dykes in the Timmiarmiit area, Southeast Greenland: evidence for a continuous Gardar swarm across Greenland's North Atlantic Craton;Bartels;GFF,2016

4. The 616Ma old Egersund basaltic dyke swarm, SW Norway, and Late Neoproterozoic opening of the Iapetus Ocean;Bingen;Journal of Geology,1998

5. The late Archean record: a puzzle in ca. 35 pieces;Bleeker;Lithos,2003

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