Show simple item record

dc.contributor.author Oddy, Richard William en_US
dc.date.accessioned 2012-05-09T20:17:08Z
dc.date.available 2012-05-09T20:17:08Z
dc.date.issued 1966 en_US
dc.identifier ocm72795046 en_US
dc.identifier.uri http://hdl.handle.net/1993/5408
dc.description.abstract Trace quantities of copper, zinc, and molybdenum have been determined in the Cretaceous beds of Manitoba. The contents of the metals are in the ranges: copper, 2 to 78 p.p.m.; zinc 5 to over 400 p.p.m.; and molybdenum, less than 2.5 to 180 p.p.m. The results indicate an enrichment of molybdenum in the Cretaceous beds and it is suggested that adsorption of molybdenum from sea water by clay minerals and organic matter in the shales, and by clay minerals in the bentonites is responsible for the enrichment. In order for such extensive enrichment the sea water must have contained an abundance of available molybdenum and the likely source of the excessive molybdenum in the sea water is Precambrian rocks in the shield area to the east. The Cretaceous beds contain normal concentrations of copper and zinc but the bentonite layers contain much lower concentrations of copper and zinc than the interbedded shales. Molybdenum poisoning of cattle in Swan River Valley is the result of the abundance of molybdenum in the Favel beds from which the soils in the valley were derived. en_US
dc.format.extent v, 36 leaves : en_US
dc.language en en_US
dc.rights en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title Trace elements in cretaceous rocks of Manitoba en_US
dc.type info:eu-repo/semantics/masterThesis
dc.degree.discipline Geology en_US


Files in this item

This item appears in the following Collection(s)

Show simple item record

View Statistics