Results 171 to 180 of about 14,415 (244)

"Melilite" in kimberlites

International Kimberlite Conference Extended Abstracts: 1998, 2019
openaire   +2 more sources

Zoning of kimberlite provinces and evolution of kimberlite magmatism

International Kimberlite Conference Extended Abstracts: 1995, 2019
openaire   +2 more sources

Polydopamine functionalized FeTiO₃ nanohexagons for selective and simultaneous electrochemical determination of dopamine and uric acid. [PDF]

RSC Adv
Aparna TK, D ST, Dar MA, Gul R, Sivasubramanian R.   +4 more
europepmc   +1 more source

Heavy potassium isotopes in carbonatites reveal oceanic crust subduction as the driver of deep carbon cycling. [PDF]

Sci Adv
Long ZY, Moynier F, Debret B, Qiu KF, Dai W, Sun HX, Deng J, Bertrand H, Burton K, Inglis E, Tappe S.   +10 more
europepmc   +1 more source

Experimental Study of a kimberlite at Pressures between 42 and 88 Kilobars [PDF]

Ito, Keisuke, Kawai, Naoto, Matsumoto, Takashi   +2 more
core  

Kimberlites des prairies

, 1996
openaire   +1 more source

Some of the next articles are maybe not open access.

Related searches:

Kimberlites

1986
R. Mitchell
openaire   +2 more sources

Indian kimberlites and the genesis of kimberlites

Chemical Geology, 1984
Abstract Late Proterozoic kimberlites occur in both southern and central India. They are similar in petrography and geochemistry to the kimberlites of southern Africa and Yakutia, U.S.S.R. These rocks contain low-CaO forsteritic olivines (Fo92), abundant phlogopites, magnesian ilmenites, aluminous—magnesian chromites, chrome-pyrope garnets surrounded
Eric A.K. Middlemost, Dalim K. Paul
openaire   +1 more source

Kimberlites: From Deep Earth to Diamond Mines

Elements, 2019
Kimberlites are rare, enigmatic, low-volume igneous rocks. They are highly enriched in magnesium, volatiles (CO2 and H2O) and incompatible trace elements and are thought to be the most deeply derived (>150 km) magmatic rocks on Earth.
A. Giuliani, D. Pearson
semanticscholar   +1 more source