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Configuration of the Late Paleoproterozoic Supercontinent Columbia: Insights from radiating mafic dyke swarms

Hou, Guiting; Santosh, M.; Qian, Xianglin; Lister, Gordon; Li, Jianghai


Remnants of 2.1-1.8 Ga orogens can be recognized in nearly every craton assembled within reconstructions of the Rodinia supercontinent, although no particular pattern of laterally extensive orogenic belts emerges. These cratons may be the fragments of an

CollectionsANU Research Publications
Date published: 2008
Type: Journal article
Source: Gondwana Research
DOI: 10.1016/


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