Search
Now showing items 1-7 of 7
Geology and geochemistry of the Laird Lake property and associated gold mineralization, Red Lake greenstone belt, northwestern Ontario
(2018)
The Laird Lake property encompasses the tectonic contact between the Balmer (2.99 to 2.96 Ga)
and the Confederation (2.74 to 2.73 Ga) assemblages on the south-western end of the Red Lake
greenstone belt, Northwestern ...
Geochemistry of shallow and deep water archean meta-iron formations and their post-depositional alteration in western Superior Province, Canada
(2018)
One purpose for studying banded meta-iron formations is to determine the chemical composition of
seawater in the Archean ocean and the oxygen content of the Archean oceanic-atmospheric system.
Geologists use the geochemistry ...
Petrogenesis of the ferrogabbroic intrusions and associated Fe-Ti-V-P mineralization within the McFaulds Greenstone belt, Superior Province, Canada
The McFaulds Lake area (commonly known as the Ring of Fire), has been the site of
much recent exploration within northern Ontario. The area represents a recently discovered
Archean greenstone belt which is host to world ...
Geochemistry and mineralization of the Archean Titan (Roaring River) intrusion, Thunder Bay, Ontario
(2023)
The 2690 ± 3.2 Ma Titan intrusion is an approximately 7 by 3 km, roughly ovoid,
mafic-ultramafic intrusion, located just north of the inferred boundary between the
Winnipeg River and Marmion terranes. Outcrop in the area ...
Geology and geochemistry of the Terrace Bay batholith, N. Ontario
(2019)
The Terrace Bay Batholith is a 25 km long oval shaped granitoid intrusion located in the
western portion of the Schreiber-Hemlo greenstone belt, part of the larger Wawa-Abitibi terrane.
The pluton was emplaced at 2689±1.1 ...
Mineral chemistry, hyperspectral analysis and applications for regional exploration at the Hemlo Gold deposit, Ontario, Canada
(2018)
The Barrick Gold owned Hemlo Au deposit is a world class Archean Au deposit situated
in Northern Ontario, Canada with historic production of >21 Moz of Au over 32 years of
continuous operation. The deposit has a strike ...
A comparison of the hydrothermal alteration systems around the Mo-hosting White Pine intrusion, Utah, and the Buckingham Porphyry, Nevada
(2015)
The White Pine Fork Mo porphyry has an estimated resource of 16 Mt of Mo at 0.1%
Mo. The host intrusions are K-feldspar- and quartz-porphyritic monzo- to syeno-granites
characterised by LREE enrichment, fractionated HREEs ...