Wood ash, the byproduct of bioenergy production from biomass, is typically discarded into landfills as waste. Adding ash back to soil may supply nutrients to soil that are lost through biomass harvesting, increase soil ...

As part of the greater Slave Province geophysical, surficial materials and permafrost study, a Northwest Territories Geological Survey (NTGS) led government-academic-industry research program, this study is intended to ...

The 2.857±5 Ga (this study) carbonate platform at Woman Lake, Ontario, Canada, presents a unique opportunity to fill a 130 million year knowledge gap on early carbonate sedimentology and ocean chemistry between similar ...

The Wabigoon subprovince is a 900 km long by 150 km wide Archean-aged granite greenstone belt. Large, synvolcanic batholiths with smaller late to post-tectonic stocks cut the numerous greenstone belts of the subprovince. ...

The Pemberton Hills study site is situated in northern Vancouver Island, British Columbia, and forms part of a northwest trending belt of porphyry deposits and prospects within the Wrangellia Terrane. The study site is ...

As the Canadian biomass energy sector grows, so too does its production of by-products such as wood ash from the combustion of wood biomass for energy. Wood ash can be land applied with the goal of increasing the ...

The Good Hope carbonatite is located northwest of Marathon, Ontario (49° 02’ N, 86° 43’ W). It occurs along the northwest margin of the Prairie Lake complex. The objectives of this research are to characterize the carbonate ...

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 ...

The eastern Sunda arc is one of the most prospective Cu-Au magmatic belts in the world with four world class copper-gold porphyry deposits: Batu Hijau (1.64 Gt at 0.44% Cu, 0.35 g/t Au), Elang (2.42 Gt at 0.31% Cu, 0.33 ...

The Escape intrusion is a tabular to bladed, mafic–ultramafic chonolith that hosts economic concentrations of PGE–Cu–Ni magmatic sulfide mineralization. The Mesoproterozoic intrusion is located about 50 km northeast of ...