NJG64-3-01
1984
The significance of a thrust fault lineation in the Kalak Nappe Complex of Finnmark
64
3
173-179

An unusual mineral lineation formed by garnets being gouged into quartzites at the base of a major nappe during late shearing shows that the nappe translation direction did not change significantly during the formation of D2 to D4 folds. This has considerable significance when correlating deformation phases to separate periods within the Caledonian orogenic event.

0029-196X
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