Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4715978 | Lithos | 2014 | 19 Pages |
Abstract
This model accounts for the differences between Fe-K suites, such as the Matok pluton, and Mg-K suites, such as sanukitoids, the origin of which only requires metasomatized mantle. We propose that the most appropriate geodynamic setting for the interaction between enriched lithospheric and asthenospheric mantle sources is an episode of “lithospheric reworking” (through slab breakoff, retreat or sub-continental mantle delamination) in response to continental collision. Depending on the relative contribution of the two mantle sources in this environment, the resulting magmas can show a wide range of compositions from Fe-K to Mg-K end-members. From a regional point of view, this conclusion supports that the Kaapvaal Craton and the Central Zone of the Limpopo Belt were amalgamated between 2.80 and 2.75Â Ga owing to continent-continent collision.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
O. Laurent, M. Rapopo, G. Stevens, J.F. Moyen, H. Martin, R. Doucelance, C. Bosq,