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Crystallogenesis and Mineralogy
Saint Petersburg, Russia
30 September-4 October 2007
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Conferences & Meetings 2nd International Conference "Crystallogenesis and Mineralogy"
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Mineralogical indicators of tectonic deformations in Verkhnekamskoe deposit of salts

RMS-DPI code:  2007-1-161-0
Scientific session:  Session 5. Crystal chemistry and crystal morphology of minerals
Author listing:  Tchaikovskiy I.I.
Principal author:  Chaikovskiy Ilya Ivanovich
Language:  Russian
Abstract - Summary 
(short description):
Morphology, structure and composition of epigenetic mineralizations are caused by position in tectonic structure of Verhnekamskoe deposit of salts. Neogenic phases are identical to structure of accommodating rocks that fends the local nature of fluids. They are dated for shear-zones and adjoining them fracture-separation. Bands of fluid-kataklaz salts, recrystallization and lenticular bodies, and also brecciated-zones and replacements-zones are formed in shear-zones. The first are formed practically in the dry conditions, the second Ц in salt brines presence, and the third are caused by migration of the water-mud suspension provoking displacement of beddings, recrystallization and halitization of potassium rocks. In fractures and cavities of separations are formed parallel-polly aggregate healings seams in boudined bands of clay, and also mineral fillings of concordant near-vault veins. Epigenetic mineralizations are fends layers character of current of salts instead of halokinez and fracture tectonics.
 
RMS-DPI code:  2007-1-161-0
Proceeedings volume 
in the RMS catalogue:
 
Crystallogenesis and Mineralogy
Pages:  368-371
File of proceedings 
(PDF): 
 284 K
Status:  printed
Accepted:  31/05/2007
Published on-line:  05/01/2008
Permanent address of publication:  http://www.minsoc.ru/2007-1-161-0/
Contact author(s):  Tchaikovskiy, Ilya Ivanovich
 

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