diamondiferous mass-flow and traction current deposits in a neoarchean fan delta, wawa area, superior province
| dc.contributor.advisor | hollings, peter | |
| dc.contributor.advisor | fralick, philip | |
| dc.contributor.author | wendland, corey | |
| dc.date.accessioned | 2012-11-10t19:17:18z | |
| dc.date.available | 2012-11-10t19:17:18z | |
| dc.date.created | 2010-05 | |
| dc.date.issued | 2012-11-10 | |
| dc.identifier.uri | http://knowledgecommons.lakeheadu.ca/handle/2453/158 | |
| dc.description.abstract | diamond bearing neoarchean metaconglomerates are present in the michipicoten greenstone belt, wawa-abitibi subprovince near wawa, ontario. they form a portion of the dore metasedimentary rocks in the arliss lake subbasin, and unconformably overlie a succession of mafic metabasalts. the conglomerates are transitional into argillite which in turn is conformably overlain by metabasalts. the conglomeratic succession has a maximum thickness of 454 meters and confined to what appears to be a deformed paleovalley at the base of the sedimentary succession. | en_us |
| dc.language.iso | en_us | en_us |
| dc.subject | diamond deposits | en_us |
| dc.subject | ontario | en_us |
| dc.subject | wawa region | en_us |
| dc.subject | northeastern | en_us |
| dc.subject | mineralogy | en_us |
| dc.subject | geology | en_us |
| dc.subject | lithofacies | en_us |
| dc.subject | geochemistries | en_us |
| dc.title | diamondiferous mass-flow and traction current deposits in a neoarchean fan delta, wawa area, superior province | en_us |
| dc.type | thesis | en_us |
| etd.degree.name | master of science | en_us |
| etd.degree.level | master | en_us |
| etd.degree.discipline | geology | en_us |
| etd.degree.grantor | 阿根廷vs墨西哥竞猜 | en_us |
