Boothia Felix, of Sheriff Booth of London fame, and Melville Peninsular of Dundas, Viscount Melville. Both have some seds, but Melville is metamorphs, and volcs more. IMHO it means that late kimberlites may survive weller, but early ones are more doubtfuler. On the other hand, what was erosion in the far white north? Glaciers did not scour, nor rain fall that much, though frost heaved. Land was not high. Many sed outliers survived. We are not sure about 1.8 billion years ago, as the arctic was not in the artic then, but somewhere in the southwest altantic-pacific all stuck together with a lot of other clods. What surging rifts and continental hangups or orogenies tropical of weather, we can only surmise. Somewhere up there is an enchanted rock-ed forest, proving that rock is truly around the clock.
Rankin-Baker-Chesterfield is some shear ain't it? Been following that one since 1995 or thereabouts. Some paraller zones I warrant. There are high NW structures, and NE too. I like to move with the continents along parallel-to-movement transform faults, near the craton edge. At least your kimbers thusly may have the same characteristics as they plumb the hotspots the continent passes, in like manner. (W.J Atkinson, Namibia)
jrhana and we are starting a diamond mining company. We plan to call it Polar Bear Wee-Wee mines Limited. Our strategy is to start diamond mining right away. This curcumvents too much expenditure on exploration. Start looking for kimberlite and you may lose track, as they can take a lot of finding. start mining however and the money rolls in.
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