Bedrock model of the Kivetty area: Summary report

Pauli Saksa; Seppo Paulamäki; Markku Paananen; Pekka Anttila; Henry Ahokas; Kai Front; Petteri Pitkänen; Juhani Korkealaakso; Olli Okko

Bedrock model of the Kivetty area: Summary report

Pauli Saksa (Editor), Seppo Paulamäki, Markku Paananen, Pekka Anttila, Henry Ahokas, Kai Front, Petteri Pitkänen, Juhani Korkealaakso, Olli Okko

Research output: Book/Report › Report

Abstract

Preliminary site investigations were carried out at Kivetty (in Finland), in 1987-1992 in accordance with the investigation programme drawn up by Teollisuuden Voima Oy (TVO). The site was modelled in terms of rock type, fracturing, fracture structures and geohydrological conditions, with the main emphasis being placed on fracturing and associated hydraulic conductivity. The various properties of the bedrock structures were classified in relation to a three-dimensional model. The descriptions of the models were stored in a computer system for the purpose of illustration. The principal rock types encountered at the Kivetty site are porphyritic granodiorite and porphyritic granite, in addition to which even-grained granite and granodiorite, gabbro, and small felsic and mafic veins occur. The rocks have undergone two distinct phases of deformation.

Original language	English
Place of Publication	Helsinki
Publisher	Voimayhtiöiden ydinjätetoimikunta
Number of pages	117
Publication status	Published - 1993
MoE publication type	D4 Published development or research report or study

Publication series

Series	YJT Report
Number	93-16
ISSN	0359-548X

Cite this

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abstract = "Preliminary site investigations were carried out at Kivetty (in Finland), in 1987-1992 in accordance with the investigation programme drawn up by Teollisuuden Voima Oy (TVO). The site was modelled in terms of rock type, fracturing, fracture structures and geohydrological conditions, with the main emphasis being placed on fracturing and associated hydraulic conductivity. The various properties of the bedrock structures were classified in relation to a three-dimensional model. The descriptions of the models were stored in a computer system for the purpose of illustration. The principal rock types encountered at the Kivetty site are porphyritic granodiorite and porphyritic granite, in addition to which even-grained granite and granodiorite, gabbro, and small felsic and mafic veins occur. The rocks have undergone two distinct phases of deformation.",

author = "Seppo Paulam{\"a}ki and Markku Paananen and Pekka Anttila and Henry Ahokas and Kai Front and Petteri Pitk{\"a}nen and Juhani Korkealaakso and Olli Okko",

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T2 - Summary report

AU - Paulamäki, Seppo

AU - Paananen, Markku

AU - Anttila, Pekka

AU - Ahokas, Henry

AU - Front, Kai

AU - Pitkänen, Petteri

AU - Korkealaakso, Juhani

AU - Okko, Olli

A2 - Saksa, Pauli

PY - 1993

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N2 - Preliminary site investigations were carried out at Kivetty (in Finland), in 1987-1992 in accordance with the investigation programme drawn up by Teollisuuden Voima Oy (TVO). The site was modelled in terms of rock type, fracturing, fracture structures and geohydrological conditions, with the main emphasis being placed on fracturing and associated hydraulic conductivity. The various properties of the bedrock structures were classified in relation to a three-dimensional model. The descriptions of the models were stored in a computer system for the purpose of illustration. The principal rock types encountered at the Kivetty site are porphyritic granodiorite and porphyritic granite, in addition to which even-grained granite and granodiorite, gabbro, and small felsic and mafic veins occur. The rocks have undergone two distinct phases of deformation.

AB - Preliminary site investigations were carried out at Kivetty (in Finland), in 1987-1992 in accordance with the investigation programme drawn up by Teollisuuden Voima Oy (TVO). The site was modelled in terms of rock type, fracturing, fracture structures and geohydrological conditions, with the main emphasis being placed on fracturing and associated hydraulic conductivity. The various properties of the bedrock structures were classified in relation to a three-dimensional model. The descriptions of the models were stored in a computer system for the purpose of illustration. The principal rock types encountered at the Kivetty site are porphyritic granodiorite and porphyritic granite, in addition to which even-grained granite and granodiorite, gabbro, and small felsic and mafic veins occur. The rocks have undergone two distinct phases of deformation.

M3 - Report

T3 - YJT Report

BT - Bedrock model of the Kivetty area

PB - Voimayhtiöiden ydinjätetoimikunta

CY - Helsinki

ER -

Bedrock model of the Kivetty area: Summary report

Abstract

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