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Characterization of crystalline rocks in deep boreholes. The Kola, Krivoy Rog and Tyrnauz boreholes. NEDRA - scientific industrial company on superdeep drilling and comprehensive investigation of the earths interior

Abstract

SKB studies, as one alternative, the feasibility of disposing of spent nuclear fuel in very deep boreholes. As a part of this work NEDRA has compiled geoscientific data from three superdeep boreholes within the former Soviet Union. The holes considered were: the Kola borehole, 12261 m deep and located on the Kola Peninsula, the Krivoy Rog borehole, 5000 m deep and located in Ukraine, and the Tyrnauz borehole, 4001 m deep and located between the Black Sea and the Caspian Sea. These boreholes all penetrate crystalline formations, but major differences are found when their tectonic environments are compared. Excluding the uppermost horizon affected by surface phenomena, data do not indicate any general correlation between depth and the state of rock fracturing, which is instead governed by site specific, lithological and tectonical factors. This applies also to fracture zones, which are found at similar frequencies at all depths. As opposed to the structural data, the hydrogeological and hydrochemical information reveals a vertical zonation, with clear similarities between the three boreholes. An upper zone with active circulation and fresh or slightly mineralized groundwaters reaches down 1000-2000 m. The interval from 1000-2000 m down to 4000-5000 m can be characterized as a transition  More>>
Publication Date:
Dec 01, 1992
Product Type:
Technical Report
Report Number:
SKB-TR-92-39
Reference Number:
SCA: 052002; 540250; PA: AIX-25:037437; EDB-94:079757; ERA-19:018124; NTS-94:022105; SN: 94001208128
Resource Relation:
Other Information: PBD: Dec 1992
Subject:
12 MANAGEMENT OF RADIOACTIVE AND NON-RADIOACTIVE WASTES FROM NUCLEAR FACILITIES; 54 ENVIRONMENTAL SCIENCES; ROCK-FLUID INTERACTIONS; GEOCHEMISTRY; ROCKS; GEOLOGIC FRACTURES; BOREHOLES; GEOLOGY; GROUND WATER; HYDRAULIC CONDUCTIVITY; HYDROLOGY; INTERNATIONAL COOPERATION; LIQUID FLOW; NUMERICAL DATA; RADIOACTIVE WASTE DISPOSAL; UNDERGROUND DISPOSAL; 052002; 540250; WASTE DISPOSAL AND STORAGE; SITE RESOURCE AND USE STUDIES
OSTI ID:
10152790
Research Organizations:
Swedish Nuclear Fuel and Waste Management Co., Stockholm (Sweden)
Country of Origin:
Sweden
Language:
English
Other Identifying Numbers:
Journal ID: ISSN 0284-3757; Other: ON: DE94624777; TRN: SE9400060037437
Availability:
OSTI; NTIS; INIS
Submitting Site:
SWDN
Size:
135 p.
Announcement Date:
Jul 05, 2005

Citation Formats

None. Characterization of crystalline rocks in deep boreholes. The Kola, Krivoy Rog and Tyrnauz boreholes. NEDRA - scientific industrial company on superdeep drilling and comprehensive investigation of the earths interior. Sweden: N. p., 1992. Web.
None. Characterization of crystalline rocks in deep boreholes. The Kola, Krivoy Rog and Tyrnauz boreholes. NEDRA - scientific industrial company on superdeep drilling and comprehensive investigation of the earths interior. Sweden.
None. 1992. "Characterization of crystalline rocks in deep boreholes. The Kola, Krivoy Rog and Tyrnauz boreholes. NEDRA - scientific industrial company on superdeep drilling and comprehensive investigation of the earths interior." Sweden.
@misc{etde_10152790,
title = {Characterization of crystalline rocks in deep boreholes. The Kola, Krivoy Rog and Tyrnauz boreholes. NEDRA - scientific industrial company on superdeep drilling and comprehensive investigation of the earths interior}
author = {None}
abstractNote = {SKB studies, as one alternative, the feasibility of disposing of spent nuclear fuel in very deep boreholes. As a part of this work NEDRA has compiled geoscientific data from three superdeep boreholes within the former Soviet Union. The holes considered were: the Kola borehole, 12261 m deep and located on the Kola Peninsula, the Krivoy Rog borehole, 5000 m deep and located in Ukraine, and the Tyrnauz borehole, 4001 m deep and located between the Black Sea and the Caspian Sea. These boreholes all penetrate crystalline formations, but major differences are found when their tectonic environments are compared. Excluding the uppermost horizon affected by surface phenomena, data do not indicate any general correlation between depth and the state of rock fracturing, which is instead governed by site specific, lithological and tectonical factors. This applies also to fracture zones, which are found at similar frequencies at all depths. As opposed to the structural data, the hydrogeological and hydrochemical information reveals a vertical zonation, with clear similarities between the three boreholes. An upper zone with active circulation and fresh or slightly mineralized groundwaters reaches down 1000-2000 m. The interval from 1000-2000 m down to 4000-5000 m can be characterized as a transition zone with lower circulation rates and gradually increasing mineralisation. Below 4000-5000 m, strongly mineralized, stagnant, juvenile or metamorphogenic waters are found. Geothermal data verify the existence of this zonation. 28 figs, 30 tabs.}
place = {Sweden}
year = {1992}
month = {Dec}
}