Mineralogical evidence for an ophiolite from the Outokumpu serpentinites in North Karelia, Finland
The serpentinites of the Outokumpu complex located in the early Proterozoic schist belt of North Karelia in Eastern Finland are investigated petrographically, mineralogically and chemically, with an emphasis on relict minerals, especially chrome spinel, and also olivine and orthopyroxene. The relict...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Geological Society of Finland
1989-06-01
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Series: | Bulletin of the Geological Society of Finland |
Subjects: | |
Online Access: | http://www.geologinenseura.fi/bulletin/Volume61/sgs_bt_061_1_pages_095_112.pdf |