Published 1976 | Version v1
Book

Regional geochemical uranium prospecting in Finland

  • 1. Geological Survey of Finland, Espoo
  • 2. Helsinki Univ. (Finland)
  • 3. Technical Research Centre of Finland, Espoo

Description

Organic-rich lake sediments were sampled over a 6000-km2 area in Karelia, eastern Finland. In addition to several smaller anomalies, the investigation indicated an extended zone of anomalously high uranium in lake sediments along the contact between Karelian schists and Pre-Karelian rocks. Loss on ignition correlated with the uranium content. Two methods of calculating uranium content with respect to the organic material were investigated. The distribution of uranium in the sediments of individual lakes was studied. It was found that central lake samples may fail to indicated isolated mineralizations in adjacent bedrock. A comparison between lake and stream sediments indicated that stream sediments may be used to complement lake sediment grids in areas of low lake density. (author)

Part of:
Existing and new techniques in uranium exploration

Additional details

Publishing Information

Publisher
IAEA.
Imprint Place
Vienna
ISBN
92-0-040076-0
Imprint Title
Exploration for uranium ore deposits
Imprint Pagination
p. 283-295.
Series
Proceedings series.

Conference

Title
Symposium on exploration of uranium ore deposits.
Dates
29 Mar - 2 Apr 1976.
Place
Vienna, Austria.

INIS

Country of Publication
International Atomic Energy Agency (IAEA)
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
8315156
Subject category
S58: GEOSCIENCES;
Resource subtype / Literary indicator
Conference
Descriptors DEI
AERIAL PROSPECTING; FINLAND; GEOLOGIC DEPOSITS; GEOLOGIC SURVEYS; LAKES; MANGANESE; MAPS; NEUTRON DETECTORS; ORGANIC COMPOUNDS; ROCKS; SAMPLING; SEDIMENTS; URANIUM; URANIUM ORES
Descriptors DEC
ACTINIDES; ELEMENTS; EUROPE; MEASURING INSTRUMENTS; METALS; ORES; PROSPECTING; RADIATION DETECTORS; SCANDINAVIA; SURFACE WATERS; TRANSITION ELEMENTS

Optional Information

Secondary number(s)
IAEA-SM--208/26.