A Tectonic Study of Mt. Nuolja, Swedish Lapland
- 1 November 1955
- journal article
- research article
- Published by Taylor & Francis in Geologiska Föreningen i Stockholm Förhandlingar
- Vol. 77 (4) , 557-566
- https://doi.org/10.1080/11035895509451752
Abstract
The overthrust Caledonian metamorphics of Mt. Nuolja are mainly S-tectonites. The dominating axial fabric elements are equivalent to B' = a of at least four phases of structogenesis. B = b of the four phases, beginning with the oldest, are: 1. N, 2. ENE, 3. NNE, 4. N.Keywords
This publication has 2 references indexed in Scilit:
- Linear structures and their relation to movement in the Caledonides of Scandinavia and ScotlandQuarterly Journal of the Geological Society, 1953
- Die Hochgebirgsbildungen am Torne Träsk in LapplandGeologiska Föreningen i Stockholm Förhandlingar, 1910