Deep-Seated Xenoliths from the Brown Breccia of the Udachnaya Pipe, Siberia

2013 ◽  
pp. 59-73 ◽  
Author(s):  
I. V. Ashchepkov ◽  
T. Ntaflos ◽  
S. S. Kuligin ◽  
E. V. Malygina ◽  
A. M. Agashev ◽  
...  
Keyword(s):  
Udachnaya Pipe

Causes of variations in morphology and impurities of diamonds from the Udachnaya Pipe eclogite

2007 ◽  
Vol 48 (9) ◽  
pp. 758-769 ◽  
Author(s):  
A.S. Stepanov ◽  
V.S. Shatsky ◽  
D.A. Zedgenizov ◽  
N.V. Sobolev
Keyword(s):  
Udachnaya Pipe

Chloride-carbonate nodules in kimberlites from the Udachnaya pipe: Alternative approach to the evolution of kimberlite magmas

2006 ◽  
Vol 44 (9) ◽  
pp. 935-940 ◽  
Author(s):  
V. S. Kamenetsky ◽  
V. V. Sharygin ◽  
M. B. Kamenetsky ◽  
A. V. Golovin
Keyword(s):  
Udachnaya Pipe ◽  
Alternative Approach

Sulfur isotopic compositions of the lithospheric mantle sulfides from the Udachnaya pipe (Yakutia)

2020 ◽  
Author(s):  
Olga Ilyina ◽  
Alexey Agashev ◽  
Bertrand Moine
Keyword(s):  
Lithospheric Mantle ◽  
Sulfur Isotopes ◽  
Basic Research ◽  
Kimberlite Pipe ◽  
West African ◽  
Udachnaya Pipe ◽  
Depleted Mantle ◽  
Isotope Ratio Mass Spectrometer ◽  
Isotope Study

<p>Sulfide inclusions in Neoproterozoic West African diamonds have revealed mass-independently fractionated sulfur isotopes in them [Smit et.al., 2019]. This feature is a sign of Archean surface changes traced in the mantle. Here we present an S isotope study of the unique fresh mantle deep-seated peridotites, eclogites and pyroxenites with rare or without any secondary alterations from the Udachnaya-East pipe. This research will give better understanding the role of subduction in the formation of the lithospheric mantle under the Siberian craton. Sulfur isotopes (<sup>34</sup>S/<sup>32</sup>S which is denoted as δ<sup>34</sup>S) were measured in the sulfides from eclogites, peridotites and pyroxenites using an Isoprime isotope ratio mass spectrometer (IRMS) with classic configuration with 4 collectors. The sulfides from eclogites are pyrrotite, pentlandites and chalcopyrites. They have δ<sup>34</sup>S values from +0,67 to +3,08 per mil (‰). Sulfides in peridotites are pyrrotite-pentlandite-chalcopyrites assemblages and they have δ<sup>34</sup>S values from +0,22 to +3,55 ‰. These δ<sup>34</sup>S values from eclogites and peridotites are broadly overlap with the field for depleted mantle and chondrites (-1,9 to +0,35‰) [Labidi et.al., 2013; 2014]. Sulfides from pyroxenites are pyrrotite and they have δ<sup>34</sup>S values from -3,62 to +1,49 ‰. These δ<sup>34</sup>S values have a wider range than the estimates for depleted mantle. The δ<sup>34</sup>S values in our samples are close to those in the depleted mantle, but still have deviation from it and do not fractionated. Our data did not detect mass-independently fractionated sulfur isotopes in the mantle samples from the Udachnaya pipe. Thus subduction of the earth’s crust did not play role in the values of sulfur isotopes of the lithospheric mantle sampled by Udachnaya kimberlite pipe. The source of sulfur in these rocks probably was the astenospheric mantle.</p><p>References</p><ol><li>Smit et. al., 2019</li> <li>Labidi et. al., 2013; 2014</li> </ol><p>This study was supported by the Russian Foundation for Basic Research № 18-05-70064</p>

Substantiation of Protective Cushion Thickness in Mining under Open Pit Bottom with the Caving Methods at Udachnaya Pipe

2018 ◽  
Vol 54 (2) ◽  
pp. 226-236
Author(s):  
I. V. Sokolov ◽  
A. A. Smirnov ◽  
Yu. G. Antipin ◽  
I. V. Nikitin ◽  
M. V. Tishkov
Keyword(s):  
Open Pit ◽  
Udachnaya Pipe

Alkali carbonates and sulfides in kimberlite-hosted chloride-carbonate nodules (Udachnaya pipe, Russia)

2006 ◽  
Vol 70 (18) ◽  
pp. A576
Author(s):  
V.V. Sharygin ◽  
V.S. Kamenetsky ◽  
M.B. Kamenetsky
Keyword(s):  
Udachnaya Pipe

Water content in minerals of mantle xenoliths from the Udachnaya pipe kimberlites (Yakutia)

2014 ◽  
Vol 55 (4) ◽  
pp. 428-442 ◽  
Author(s):  
A.L. Ragozin ◽  
A.A. Karimova ◽  
K.D. Litasov ◽  
D.A. Zedgenizov ◽  
V.S. Shatsky
Keyword(s):  
Water Content ◽  
Mantle Xenoliths ◽  
Udachnaya Pipe
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