Publications of D. V. Kuzmin
All genres
Journal Article (34)
21.
Journal Article
50 (12), pp. 999 - 1033 (2009)
Siberian meimechites: origin and relation to flood basalts and kimberlites. Russian Geology and Geophysics 22.
Journal Article
112 (Supplement 2), pp. 701 - 713 (2009)
Petrogenetic significance of minor elements in olivines from diamonds and peridotite xenoliths from kimberlites of Yakutia. Lithos 23.
Journal Article
17 (3), pp. 253 - 286 (2009)
Petrology of the parental melts and mantle sources of Siberian trap magmatism. Petrology 24.
Journal Article
28, pp. 53 - 68 (2009)
Laser ablation-inductively coupled plasma mass spectrometry and its application in geochemistry, cosmochemistry and environmental research. Rock and Mineral Analysis (China) 25.
Journal Article
24 (9), pp. 1237 - 1243 (2009)
In situ Sr isotopic analysis of low Sr silicates using LA-ICP-MS. Journal of Analytical Atomic Spectrometry 26.
Journal Article
456 (7218), pp. 89 - 92 (2008)
The Earth's missing lead may not be in the core. Nature 27.
Journal Article
321 (5888), p. 536 - 536 (2008)
A quantitative link between recycling and osmium isotopes. Science 28.
Journal Article
49 (4), pp. 823 - 839 (2008)
Olivine in the udachnaya-east kimberlite (Yakutia, Russia): Types, compositions and origins. Journal of Petrology 29.
Journal Article
32 (1), pp. 5 - 26 (2008)
An automated iridium-strip heater for LA-ICP-MS bulk analysis of geological samples. Geostandards and Geoanalytical Research 30.
Journal Article
20, pp. 305 - 315 (2008)
Olivine inclusions in Siberian diamonds: high-precision approach to minor elements. European Journal of Mineralogy 31.
Journal Article
46 (1), pp. 1 - 16 (2008)
Conditions of quaternary magmatism at Spitsbergen Island. Geochemistry International 32.
Journal Article
449 (7161), pp. 456 - 458 (2007)
Metal saturation in the upper mantle. Nature 33.
Journal Article
316 (5823), pp. 412 - 417 (2007)
The amount of recycled crust in sources of mantle-derived melts. Science 34.
Journal Article
35 (3), pp. 255 - 258 (2007)
Arrival of extremely volatile-rich high-Mg magmas changes explosivity of Mount Etna. Geology