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Publikováno v:
Canadian Journal of Earth Sciences. 25:528-546
During the early Proterozoic, the 2 km thick differentiated gabbroic Kiernan sills were emplaced into a thick accumulation of pillow basalt and associated deep-water strata, the Hemlock Formation, in the southern Lake Superior region. On the basis of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e40d000df8aac12d2707fb5dd7284d7b
https://doi.org/10.1139/e88-052
https://doi.org/10.1139/e88-052
