Abstract
Preliminary site investigations implemented in accordance with the research programme drawn up by Teollisuuden Voima Oy (TVO) were carried out at Syyry (in Finland) in 1987-1992. Models of the site were compiled and used for describing the rock types, fracturing, fracture structures and geohydrological conditions, the main emphasis being on the examination of the bedrock fracturing and related hydraulic conductivity. Three-dimensional models were used for the classification of the various properties of the bedrock structures. The descriptive models were gathered into a computer system to facilitate illustration and storage. The main rock type at Syyry is tonalite. A mica gneiss formation SE of the investigation site dips towards the NW and delimits the tonalite as far as the central part of the investigation site. The miga gneiss has a heterogeneous composition and includes intermediate layers consisting of quartz feldspar schist and amphibolite. There are mafic formations in the vicinity of the investigation site. The intrusive rocks have been deformed during three plastic and three mainly brittle deformation stages. (47 refs., 61 figs.).
Saksa, P;
[1]
Ahokas, H;
[2]
Kuivamaeki, A;
Kurimo, M;
Paananen, M;
[3]
Anttila, P;
[4]
Front, K;
Pitkaenen, P;
Hassinen, P;
Ylinen, A
[5]
- ed.
- Fintact Ky, Helsinki (Finland)
- Geological Survey of Finland, Espoo (Finland)
- IVO International Oy, Vantaa (Finland)
- Technical Research Centre of Finland, Espoo (Finland). Road, Traffic and Geotechnical Lab.
Citation Formats
Saksa, P, Ahokas, H, Kuivamaeki, A, Kurimo, M, Paananen, M, Anttila, P, Front, K, Pitkaenen, P, Hassinen, P, and Ylinen, A.
Bedrock Model of the Syyry area. Summary report.
Finland: N. p.,
1993.
Web.
Saksa, P, Ahokas, H, Kuivamaeki, A, Kurimo, M, Paananen, M, Anttila, P, Front, K, Pitkaenen, P, Hassinen, P, & Ylinen, A.
Bedrock Model of the Syyry area. Summary report.
Finland.
Saksa, P, Ahokas, H, Kuivamaeki, A, Kurimo, M, Paananen, M, Anttila, P, Front, K, Pitkaenen, P, Hassinen, P, and Ylinen, A.
1993.
"Bedrock Model of the Syyry area. Summary report."
Finland.
@misc{etde_10144731,
title = {Bedrock Model of the Syyry area. Summary report}
author = {Saksa, P, Ahokas, H, Kuivamaeki, A, Kurimo, M, Paananen, M, Anttila, P, Front, K, Pitkaenen, P, Hassinen, P, and Ylinen, A}
abstractNote = {Preliminary site investigations implemented in accordance with the research programme drawn up by Teollisuuden Voima Oy (TVO) were carried out at Syyry (in Finland) in 1987-1992. Models of the site were compiled and used for describing the rock types, fracturing, fracture structures and geohydrological conditions, the main emphasis being on the examination of the bedrock fracturing and related hydraulic conductivity. Three-dimensional models were used for the classification of the various properties of the bedrock structures. The descriptive models were gathered into a computer system to facilitate illustration and storage. The main rock type at Syyry is tonalite. A mica gneiss formation SE of the investigation site dips towards the NW and delimits the tonalite as far as the central part of the investigation site. The miga gneiss has a heterogeneous composition and includes intermediate layers consisting of quartz feldspar schist and amphibolite. There are mafic formations in the vicinity of the investigation site. The intrusive rocks have been deformed during three plastic and three mainly brittle deformation stages. (47 refs., 61 figs.).}
place = {Finland}
year = {1993}
month = {Sep}
}
title = {Bedrock Model of the Syyry area. Summary report}
author = {Saksa, P, Ahokas, H, Kuivamaeki, A, Kurimo, M, Paananen, M, Anttila, P, Front, K, Pitkaenen, P, Hassinen, P, and Ylinen, A}
abstractNote = {Preliminary site investigations implemented in accordance with the research programme drawn up by Teollisuuden Voima Oy (TVO) were carried out at Syyry (in Finland) in 1987-1992. Models of the site were compiled and used for describing the rock types, fracturing, fracture structures and geohydrological conditions, the main emphasis being on the examination of the bedrock fracturing and related hydraulic conductivity. Three-dimensional models were used for the classification of the various properties of the bedrock structures. The descriptive models were gathered into a computer system to facilitate illustration and storage. The main rock type at Syyry is tonalite. A mica gneiss formation SE of the investigation site dips towards the NW and delimits the tonalite as far as the central part of the investigation site. The miga gneiss has a heterogeneous composition and includes intermediate layers consisting of quartz feldspar schist and amphibolite. There are mafic formations in the vicinity of the investigation site. The intrusive rocks have been deformed during three plastic and three mainly brittle deformation stages. (47 refs., 61 figs.).}
place = {Finland}
year = {1993}
month = {Sep}
}