Forty-two different Devonian granitoid intrusions in New Brunswick were studied for this project. They formed by crustal growth processes during the Acadian...
Two suites of felsic intrusions were emplaced during the later parts of the Appalachian orogenic cycle in New Brunswick. However, just those associated with...
The Cantung mine is a world-class W-skarn deposit; it is located just east of the Yukon border in the Selwyn Mountain Range of the Northwest Territories. The...
The Sisson Brook W-Mo-Cu deposit, situated in west-central New Brunswick, is hosted by Cambro- Ordovician volcanic and sedimentary rocks of the Miramichi and...
There are over 150 granitoid intrusions in the New Brunswick; however, all the mineralised intrusions formed in relation to Acadian and Neoacadian orogenic...
The world-class massive sulfide deposits of Zn-Pb-Cu-Ag-Au type in the Bathurst Mining Camp, Eastern Canada are hosted within Middle Ordo-vician bimodal...
Pyrite is a ubiquitous refractory sulphide mineral in massive sulphide deposits. It typically hosts minor elements, such as Cu, Ni, As, and Co, as well as many...
The Sisson deposit is a Late Devonian, structurally-controlled, intrusion-related W-Mo deposit located in west-central New Brunswick. Resources are estimated...
In the northern part of the late Archean Yellowknife Greenstone Belt, tholeiitic basalt of the Crestaurum Formation is bleached along a 7 km strike length....
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