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Deformation of metavolcanics in the Karachay Lake area, Southern Urals: petrophysical and mineral—chemical aspects

By
V. A. Petrov
V. A. Petrov
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry (IGEM), Russian Academy of Sciences, 35 Staromonetny per., Moscow 109017, Russia (e-mail: vlad@igem. ru)
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V. V. Poluektov
V. V. Poluektov
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry (IGEM), Russian Academy of Sciences, 35 Staromonetny per., Moscow 109017, Russia (e-mail: vlad@igem. ru)
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A. V. Zharikov
A. V. Zharikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry (IGEM), Russian Academy of Sciences, 35 Staromonetny per., Moscow 109017, Russia (e-mail: vlad@igem. ru)
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V. I. Velichkin
V. I. Velichkin
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry (IGEM), Russian Academy of Sciences, 35 Staromonetny per., Moscow 109017, Russia (e-mail: vlad@igem. ru)
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R. M. Nasimov
R. M. Nasimov
United Institute of Physics of the Earth (OIFZ), Russian Academy of Sciences, 10 B, Gruzinskaya Street, Moscow 123810, Russia
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N. I. Diaur
N. I. Diaur
United Institute of Physics of the Earth (OIFZ), Russian Academy of Sciences, 10 B, Gruzinskaya Street, Moscow 123810, Russia
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V. A. Terentiev
V. A. Terentiev
United Institute of Physics of the Earth (OIFZ), Russian Academy of Sciences, 10 B, Gruzinskaya Street, Moscow 123810, Russia
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V. M. Shmonov
V. M. Shmonov
Institute of Experimental Mineralogy (IEM), Russian Academy of Sciences, Chernogolovka, Moscow Region 142432, Russia
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V. M. Vitovtova
V. M. Vitovtova
Institute of Experimental Mineralogy (IEM), Russian Academy of Sciences, Chernogolovka, Moscow Region 142432, Russia
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Published:
January 01, 2005

Abstract

This paper is the result of laboratory tests aimed at comparative assessment of the filtration, elastic and mechanical properties of metavolcanics, as well as a preliminary investigation of the nature of characteristic variations in P-T parameters, simulating the conditions in the vicinity of an underground storage facility for heat-generating radioactive waste. The properties have been studied in cores collected from the deepest (1200 m) hole in the metavolcanics, focusing on intervals subjected to different strain intensities. Interpretation of the data obtained suggests that the identification of the most probable pathways for fluid flow and radionuclide transport depends on estimates of the retardation characteristics of zones of disjunctive dislocation. However, the widespread occurrence of linear zones of schistosity, mylonitization and brecciation may not be a decisive negative factor in the long-term performance assessment of the underground storage facility, because these minerals, which concentrate radionuclides such as epidote, chlorite, sericite, and Fe oxyhydroxides are widely distributed in these zones. Moreover, open microfractures and pores affected by heat will be filled with neoformed minerals (epidote, chlorite, carbonate) characterized by high sorption capacity with respect to radionuclides, due to release of intergranular water, as well as carbonatization reactions. Simultaneously, the system of open macro- and microfractures that resulted from stress affecting relatively undisturbed blocks may be one of the factors dramatically reducing country rock retention capability. Therefore, the results of petrophysical and mineral-chemical investigations must be taken into account in feasibility studies of designs for the construction of underground systems for final disposal of high-level wastes and/or long-term storage of spent nuclear fuel in the PA Mayak area.

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Contents

Geological Society, London, Special Publications

Petrophysical Properties of Crystalline Rocks

P. K. Harvey
P. K. Harvey
University of Leicester, UK
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T. S. Brewer
T. S. Brewer
University of Leicester, UK
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P. A. Pezard
P. A. Pezard
Université de Montpellier II, France
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V. A. Petrov
V. A. Petrov
IGEM, Russian Academy of Sciences, Russia
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Geological Society of London
Volume
240
ISBN electronic:
9781862394889
Publication date:
January 01, 2005

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