Olivine is the dominant component in kimberlites (~ 40–60 vol%), where it occurs as individual grains of variable size (> 1 cm to< 100 μm) of xenocrystic and magmatic origin …
Kimberlite magmatism has occurred in cratonic regions on every continent. The global age distribution suggests that this form of mantle melting has been more prominent after 1.2 Ga …
Kimberlite magmas have the deepest origin of all terrestrial magmas and are exclusively associated with cratons,,. During ascent, they travel through about 150 kilometres of cratonic …
M Tang, XL Wang, XJ Shu, D Wang, T Yang… - Earth and Planetary …, 2014 - Elsevier
We carried out a geochemical evaluation and modeled the mechanism responsible for varied Hf isotopic ratios in magmatic zircons of a single granitic rock specimen. Five …
Kimberlites are ultrabasic, Si-undersaturated, low Al, low Na rocks rich in CO2 and H2O. The distinctive geochemical character of kimberlite is strongly influenced by the nature of the …
S Tappe, RL Romer, A Stracke, A Steenfelt… - Earth and Planetary …, 2017 - Elsevier
Kimberlite and carbonatite magmas that intrude cratonic lithosphere are among the deepest probes of the terrestrial carbon cycle. Their co-existence on thick continental shields is …
Kimberlites are volatile-rich, occasionally diamond-bearing magmas that have erupted explosively at Earth's surface in the geologic past,–. These enigmatic magmas, originating …
Kimberlite magmas are of economic and scientific importance because they represent the major host to diamonds and are probably the deepest magmas from continental regions. In …
Large igneous provinces (LIPs) represent significant reservoirs of energy and metals that can either drive or contribute to a variety of metallogenic systems. The relationships between …