The Thompson Belt, also referred to as the Thompson Nickel Belt, is an Archean and early Proterozoic geologic feature in Manitoba, Canada. It contains gneiss related to deformation of the Trans-Hudson orogeny.[1]

References

  1. ^ Tectonic interpretations of systematic variations in quartz c-axis fabrics across the Thompson Belt
Allikas: https://en.wikipedia.org/wiki/Thompson_Belt
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