Origin of ultramafic–mafic bodies on the Isles of Lewis and Harris (Scotland, UK): Constraints on the Archean–Paleoproterozoic evolution of the Lewisian Gneiss Complex, North Atlantic Craton

Author:

Guice George L.,Miocevich Sophie R.,Hughes Hannah S.R.,McDonald Iain,Goodenough Kathryn M.,Ackerson Michael R.,MacDonald John M.,Faithfull John W.

Funder

Society of Economic Geologists Foundation

Christ's College, University of Cambridge

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference140 articles.

1. Emergence of peraluminous crustal magmas and implications for the early Earth;Ackerson;Geochem. Perspect. Lett.,2021

2. Fluid inclusions in Scourian granulites from the Lewisian complex of NW Scotland: evidence for CO2-rich fluid in Late Archaean high-grade metamorphism;Andersen;Lithos,1997

3. A reevaluation of Archean intracratonic terrane boundaries on the Kaapvaal Craton, South Africa: Collisional suture zones?;Anhaeusser;Geol. Soc. Am. Spec. Pap.,2006

4. Metasomatized and hybrid rocks associated with a Palaeoarchaean layered ultramafic intrusion on the Johannesburg Dome;Anhaeusser;South Africa: J. African Earth Sci.,2015

5. Arndt, N.T., 2013, Formation and Evolution of the Continental Crust: Geochemical Perspectives, v. 2, p. 405–533, doi:10.7185/geochempersp.2.3.

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