Count Iblis
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http://www.users.muohio.edu/rakovajf/WTTW%20Kimberlite.pdf"
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The discussion centers on the geological phenomenon of kimberlite eruptions, specifically their rapid ascent from depths of 250 km to the surface at speeds of approximately 70 km/hr. Unlike typical volcanic eruptions, kimberlites are characterized by their abrupt and focused nature, lacking a known mechanism for gradual movement through the mantle. The presence of ancient carbon, or diamonds, at such depths raises questions about their stability and the geological processes involved in their transport. Kimberlite eruptions have been documented across all continents, primarily in ancient shield regions, with ages ranging from the early Precambrian to recent times.
PREREQUISITESGeologists, mineralogists, and anyone interested in the dynamics of kimberlite eruptions and diamond formation will benefit from this discussion.
(kimberlite) … provides the deepest samples of the planet, because it has been erupted at high speed (roughly 70 km/hr as diamond is not stable above 150 km and will in the high heat revert in form back to carbon, if it does not move at 70 km/hr cooled by the entrapped expanding gas.) from depths in excess of 150 km (a region in which diamond is stable)
Diamondiferous kimberlite is known on all the continents, where is confined to the oldest shield segments, …
The eruptions range in age from early Precambrian to recent with a notable display in Cretaceous times in Africa and South America. No kimberlites have been recorded in the ocean basin.
From the detailed mineral chemistry it is possible to estimate the samples (Saul: Kimberlite) come from depths to about 250 km…
The ages of the diamonds are also interesting, because they are commonly much older than the host kimberlite, some, indeed, are as old as the oldest rocks on the Earth, showing that many, if not all were picked up by the kimberlite during its passage to the surface.