The O'okiep Copper District is underlain by voluminous 1035-1210 Ma granite gneiss and granite with remnants of metamorphosed supracrustal rocks. This...
Development of a microprobe technique to determine Pb isotope ratios within the growth layers of mammal teeth could have widespread applications in Pb...
Lithological and structural mapping in the east Wekusko Lake area of the Flin Flon Belt, Trans-Hudson Orogen, suggested an intimate relationship between...
The Flin Flon Belt is a complex ("Amisk collage") of distinct tectono-stratigraphic assemblages that was brought together at a relatively early stage in the...
Geochemical and isotopic (Nd, Sr) data are reported on Paleoproterozoic (1904-1864 Ma), maficintermediate (<63% SiO2), arc metavolcanic rocks from the Flin...
The Flin Flon Belt (Trans-Hudson Orogen, Manitoba and Saskatchewan) is the largest Paleoproterozoic volcanic-hosted massive sulphide (VMS) district in the...
The western Churchill Province of the Canadian Shield experienced a prolonged and complex formation history (ca. 4.04 to 1.70 Ga), with evidence for multiple...
This study investigates diagenetic and geochemical processes that control regional distribution and formation of sulfate minerals (i.e., anhydrite and barite)...
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