On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland
The Tuomivaara iron formation is an example of a chemically sedimented, strata bound occurrence of Pre-Cambrian age. It is characterized by a relatively large volume of silicate facies, while the economically important oxide facies is in a subordinate position. The general stratigraphy of the Tuomiv...
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Format: | Article |
Language: | English |
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Geological Society of Finland
1976-12-01
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Series: | Bulletin of the Geological Society of Finland |
Online Access: | http://www.geologinenseura.fi/bulletin/Volume48/sgs_bt_048_1_2_pages_071_086.pdf |
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author | K. Mäkelä |
author_facet | K. Mäkelä |
author_sort | K. Mäkelä |
collection | DOAJ |
description | The Tuomivaara iron formation is an example of a chemically sedimented, strata bound occurrence of Pre-Cambrian age. It is characterized by a relatively large volume of silicate facies, while the economically important oxide facies is in a subordinate position. The general stratigraphy of the Tuomivaara area is given, and the petrography of the iron formation horizon is described in more detail. Some economic aspects are presented. The origin of iron formations is discussed. |
first_indexed | 2024-12-10T16:53:19Z |
format | Article |
id | doaj.art-41a56c7a2a524722bd59071cfa7a4d66 |
institution | Directory Open Access Journal |
issn | 0367-5211 1799-4632 |
language | English |
last_indexed | 2024-12-10T16:53:19Z |
publishDate | 1976-12-01 |
publisher | Geological Society of Finland |
record_format | Article |
series | Bulletin of the Geological Society of Finland |
spelling | doaj.art-41a56c7a2a524722bd59071cfa7a4d662022-12-22T01:40:49ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46321976-12-01481-2718610.17741/bgsf/48.1-2.007On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern FinlandK. MäkeläThe Tuomivaara iron formation is an example of a chemically sedimented, strata bound occurrence of Pre-Cambrian age. It is characterized by a relatively large volume of silicate facies, while the economically important oxide facies is in a subordinate position. The general stratigraphy of the Tuomivaara area is given, and the petrography of the iron formation horizon is described in more detail. Some economic aspects are presented. The origin of iron formations is discussed.http://www.geologinenseura.fi/bulletin/Volume48/sgs_bt_048_1_2_pages_071_086.pdf |
spellingShingle | K. Mäkelä On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland Bulletin of the Geological Society of Finland |
title | On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland |
title_full | On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland |
title_fullStr | On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland |
title_full_unstemmed | On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland |
title_short | On the stratigraphy and petrography of the Tuomivaara iron formation in Sotkamo, northern Finland |
title_sort | on the stratigraphy and petrography of the tuomivaara iron formation in sotkamo northern finland |
url | http://www.geologinenseura.fi/bulletin/Volume48/sgs_bt_048_1_2_pages_071_086.pdf |
work_keys_str_mv | AT kmakela onthestratigraphyandpetrographyofthetuomivaaraironformationinsotkamonorthernfinland |