Dacitic ocelli in mafic lavas, 3.8–3.7 Ga Isua greenstone belt, West Greenland: Geochemical evidence for partial melting of oceanic crust and magma mixing

Author:

Appel Peter W.U.,Polat Ali,Frei Robert

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference143 articles.

1. The pre-3760 m.y. old supracrustal rocks of the Isua Area, Central West Greenland, and the associated occurrence of quartz-banded ironstone;Allaart,1976

2. Tectonic setting for the genesis of oceanic plagiogranites: evidence from a paleo-spreading structure in the Oman ophiolite;Amri;Earth Planet. Sci. Lett.,1996

3. The anatomy of an extrusive–intrusive Archean sequence: the Nelshoogte schist and Stolzburg layered ultramafic complex, Barberton greenstone belt, South Africa;Anhaeusser;S. African J. Geol.,2001

4. Recognizable primary volcanic and sedimentary features in a low strain domain of the highly deformed, oldest known (3.7–3.8 Gry) Greenstone belt, Isua, West Greenland;Appel;Terra Nova,1998

5. Textures in komatiites and variolitic basalts;Arndt,2004

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