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200th Anniversary Meeting of the Russian Mineralogical Society
Saint Petersburg, Russia
10-13 October 2017
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Detection of the magmatic activity evidence in the host rocks of the Chukuk tube (Western Yakutia) according to the X-ray and thermographic analysis

RMS-DPI code:  2017-1-101-0
Scientific session:  3. Applied mineralogy in exploration and technology.
Author listing:  Liskovaya L.V., Ignatov P.A.
Principal author:  Liskovaya Ludmila Valentihovna
Language:  Russian
Abstract - Summary 
(short description):
Annotation: For the space abutting whis the kimberlite pipe Chukukskaya (Daldyno-Alakit diamondiferous area Yakutia Alakit-Markha kimberlite field) revealed signs of secondary changes caused by the magma activities. For which the following characteristics of calcite, dolomite and carbonate rocks were used: 1) the specific heat of carbonates is Q j / g; 2) the degree of calcification and dolomitization; 3) the variability of carbonates, estimated from the relative intensity of the X-ray reflection line 113, the amount of carbonates changed and their ratio; 4) silicification; 5) chloritization and the presence of smectites, as possible products of destruction of kimberlites. The established signs are less intense than in the etalon of the near-tubular space, as the kimberlite-changing rocks of the Nyurbinskaya and Botuobinskaya pipes (the \"Alluvial-B\" facility) are chosen.
Keywords: space abutting whis the kimberlite pipe, feature of magmatic activity, kimberlite pipe, rocks hosting kimberlites, carbonates, calcite, dolomite
 
RMS-DPI code:  2017-1-101-0
Pages:  99-101
File of proceedings 
(PDF): 
 302 K
Status:  printed
Accepted:  16/09/2017
Published on-line:  07/12/2017
Permanent address of publication:  http://www.minsoc.ru/2017-1-101-0/
Contact author(s):  Liskovaya, Ludmila Valentihovna
 

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