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Additionally, the funding stream for disaster-risk reduction and climate adaptation will support structural projects, such as dikes and pump stations, with funding of as much as $5 million, increased from $2 million.
Gold mineralization is hosted within a meta-sedimentary sequence dominated by banded (graphitic) quartzite and interbedded pelitic biotite schist that is cross-cut by numerous felsic to intermediate dikes and sills.
Source: https://investingnews.com/freegold-appoints-maurice-tagami-to-board-of-directors/
Late-stage aplite, quartz feldspar porphyry and mafic dikes also occur with the mineralized zones and in outcrop.
The dikes are typically composed of Spodumene (lithium aluminium silicate in the pyroxene family) as well as accessory minerals including quartz, feldspars and micas.
“The dikes have been raised in key areas.
Source: https://globalnews.ca/news/9709395/abbotsford-teen-applauded-podcast-flood/