The results on physical properties of naturally hosting rocks and kimberlites of Arkhangel'sk diamondiferous province are considered. Geologic-geophysical model of diamond deposits of the considered field has been constructed.
V YU Abramov
doaj
Tungsten-182 evidence for an ancient kimberlite source. [PDF]
Nakanishi N +6 more
europepmc +1 more source
Sublithospheric diamond ages and the supercontinent cycle. [PDF]
Timmerman S +25 more
europepmc +1 more source
Perovskite-bearing crystal-controlled oxide-silicate mantle xenoliths: Resolution to controversial origins? [PDF]
Haggerty SE.
europepmc +1 more source
Remnants of early Earth differentiation in the deepest mantle-derived lavas. [PDF]
Giuliani A +3 more
europepmc +1 more source
Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds. [PDF]
Howarth GH +4 more
europepmc +1 more source
Linking deep CO2 outgassing to cratonic destruction. [PDF]
Wang ZX, Liu SA, Li S, Liu D, Liu J.
europepmc +1 more source
The discovery of kimberlites in Antarctica extends the vast Gondwanan cretaceous province
Kimberlites are a volumetrically minor component of the Earth's volcanic record, but are very important as the major commercial source of diamonds and as the deepest samples of the Earth's mantle. They were predominantly emplaced from =2,100 Ma to =10 ka
Nichols, GT (15580319) +6 more
core
The global distribution of CO<sub>2</sub>-rich magmas is determined by lithospheric thickness. [PDF]
Bowman EE, Gibson SA, Sui S, Lebedev S.
europepmc +1 more source
A universal concept for melting in mantle upwellings. [PDF]
Schmidt MW, Paneva N, Giuliani A.
europepmc +1 more source

