The deep mantle (2,800 km on the SMEAN tomography model) is dominated by two large low shear wave velocity provinces (LLSVPs) beneath Africa and the Pacific. The 1% slow contour (approximating to the plume generation zones) is shown as a thick red line. 80% of all reconstructed kimberlite locations (black dots) of the past 320 Myr erupted near or over the sub-African plume generation zone. The most 'anomalous' kimberlites (17%) are from Canada (white dots). Present-day continents are shown as a background, to illustrate the distribution of hotspots classified as being of deep-plume origin and present-day shear-wave velocity anomalies and bear no geographical relationship to reconstructed kimberlites or large igneous provinces.
While doing post-doctoral studies at Monash University in Melbourne Adrian Pittari studied kimberlites from Saskatchewan, Canada. These are the long-cooled remains of magma that has erupted rapidly from deep within the Earth. They are the main source of diamonds and mining companies are interested in the processes that concentrate diamonds in different parts of the kimberlite deposits, commonly known as pipes. Read more
Kimberlite is a type of potassic volcanic rock best known for sometimes containing diamonds. It is named after the town of Kimberley in South Africa, where the discovery of an 83.5-carat (16.7 g) diamond in 1871 spawned a diamond rush, eventually creating the Big Hole. Read more