The general consensus reached on kimberlites is that they are formed deep within the mantle, at between 150 and 450 kilometres depth, from anomalously enriched exotic mantle compositions, and are erupted rapidly and violently, often with considerable carbon dioxide and other volatile components.
Formation occurs at depths between, from anomalously enriched exotic mantle compositions, and are erupted rapidly and violently, often with considerable carbon dioxide and other volatile components. The general consensus on kimberlites is that they are formed deep within the mantle.
The general consensus on kimberlites is that they are formed deep within the mantle. Formation occurs at depths between, from anomalously enriched exotic mantle compositions, and are erupted rapidly and violently, often with considerable carbon dioxide and other volatile components.
The general consensus on kimberlites is that they are formed deep within the mantle. Formation occurs at depths between, from anomalously enriched exotic mantle compositions, and are erupted rapidly and violently, often with considerable carbon dioxide and other volatile components.