The Lapland greenstone belt: Stratigraphic and depositional features in northern Finland
The Lapland greenstone belt formed in a continental environment, as a result of rifting of the 3.1—3.0 Ga Saamian craton. The basin subsided to a depth of five kilometres between 3.0—2.5 Ga and contains a sequence which is subdivided into Lower, Middle and Upper Lapponian groups, with the Middle Lap...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Geological Society of Finland
1987-12-01
|
| Series: | Bulletin of the Geological Society of Finland |
| Subjects: | |
| Online Access: | http://www.geologinenseura.fi/bulletin/Volume59/sgs_bt_059_2pages_129_154.pdf |