In the pic below we can see the Wanapatei Group complex which is a stand alone , near anomaly whereas it's inclusive to itself as a rock group indifferent than it's surroundings.
In my pervious post - i suggested - even with the grenville land mass south of Wanapatei complex seen as an oval didn't - budge - but rather lands around it moved creating ripple land disturbences around it.
In this pic below - shows a zoned ovoid structure - i couldn't help but think of Wanapatei's Group structure - Wanapatei being an ovoid on a much larger scale ?
https://www.flickr.com/photos/89902546@N02/8187428244/ In this image below we can see what the Wanapatei structure is made of,
Igneous rock - magmatic - yeah... that kind of tough rock that stands to reason why it didn't budge when the grenville land mass moved northerly... just my own opinion.
Page 18 - PDF https://www.google.com/url?sa=i&url=http%3A%2F%2Fwww.geologyontario.mndmf.gov.on.ca%2Fmndmfiles%2Fpub%2Fdata%2Fimaging%2FOFR5995%2FOFR5995.pdf&psig=AOvVaw1IeFnSlAeWPrmy5GgNN77D&ust=1622994556116000&source=images&cd=vfe&ved=0CAkQjhxqFwoTCJiyv4XsgPECFQAAAAAdAAAAABAD On another note - i've been researching the Atikokan area and Quetico fault and all the other fault zones around the Hammond Reef - seeing if there's similarities to that of, Scad and Wanapatei - other similarities besides the shallow depth gold -
Cheers....