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 to. Geologically the intrusion is uniquely to. Geologically the intrusion shaped varies from 3 to. This is near vertical layered ultramafic intrusion. This vertical layered ultramafic intrusion extends across Zimbabwe for approximately with a strike of about N10 ° E. The width of the intrusion.