Geologically the intrusion is not a dyke, but is uniquely-shaped, near vertical layered ultramafic intrusion that extends across Zimbabwe for approximately with a strike of about N10 ° E. The width of the intrusion varies from 3 to.
Geologically the intrusion is not a dyke, but is lopolithic and Y-shaped in cross-section. It is a layered ultramafic intrusion that extends across Zimbabwe for approximately with a strike of about N10 ° E. The width of the intrusion varies from 3 to.