Definition
A greenstone belt is a usually an elongate structure composed dominantly of metamorphosed volcanic and sedimentary rocks that, together with granitoids and gneiss, are the constituents of Archean and Proterozoic cratons. The volcanic rocks range in composition from komatiite to rhyolite but are dominated by basalt; sedimentary rock types include shale, quartzite, sandstone, and chert. Geochemical compositions of the basaltic rocks show that some formed as oceanic crust, perhaps as part of oceanic plateaux and others formed in island arcs. Although the metamorphic grade ranges from sub-greenschist to amphibolite facies, greenschist facies dominates. Abundant chlorite and actinolite in greenschist-faciesbasalts imparts a green color that gives rise to the name greenstone belt. Most units are steeply dipping, tightly folded, and cut in places by large shear zones, which develop as the belts are accreted to the continent following their generation in oceanic crustal or arc...
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2011 Springer-Verlag Berlin Heidelberg
About this entry
Cite this entry
Arndt, N. (2011). Greenstone Belts. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-11274-4_676
Download citation
DOI: https://doi.org/10.1007/978-3-642-11274-4_676
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-11271-3
Online ISBN: 978-3-642-11274-4
eBook Packages: Physics and AstronomyReference Module Physical and Materials ScienceReference Module Chemistry, Materials and Physics