Published 1996 | Version v1
Report Restricted

Silicate geothermometry as an indicator of water-rock interaction processes in the serpentinized mafic-ultramafic intrusion of Ylivieska

Creators

  • 1. Geological Survey of Finland, Espoo (Finland)
  • 2. Univ. of Waterloo (Canada)

Description

The aim of the study was to use oxygen and hydrogen isotopes to examine the origin of different generations of serpentine. Of special interest was the study of low-temperature generations that may be correlated with the present meteoric waters. The research was commenced with drill core logging in order to obtain insight into the fracture minerals and their distribution in a mafic-ultramafic intrusion. (39 refs., 17 figs., 5 tabs.)

Availability note (English)

MF available from INIS under the Report Number.

Files

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Additional details

Publishing Information

ISBN
951-690-634-6
Imprint Pagination
39 p.
Report number
GTK-YST--94

INIS

Country of Publication
Finland
Country of Input or Organization
Finland
INIS RN
28049103
Subject category
S58: GEOSCIENCES; S58: GEOSCIENCES; S12: MANAGEMENT OF RADIOACTIVE WASTES, AND NON-RADIOACTIVE WASTES FROM NUCLEAR FACILITIES;
Descriptors DEI
FINLAND; GEOLOGIC FRACTURES; GROUND WATER; HYDROGEN ISOTOPES; MINERALS; OXYGEN ISOTOPES; ROCK-FLUID INTERACTIONS; SILICATES; TEMPERATURE MEASUREMENT
Descriptors DEC
DEVELOPED COUNTRIES; EUROPE; GEOLOGIC STRUCTURES; HYDROGEN COMPOUNDS; OXYGEN COMPOUNDS; SCANDINAVIA; SILICON COMPOUNDS; WATER; WESTERN EUROPE

Optional Information

Notes
Nuclear Waste Disposal Research.