Resurgent strike-slip duplex development along the Hitra-Snåsa and Verran Faults, Møre-trøndelag fault zone, Central Norway
- 1 January 1989
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 11 (3) , 295-305
- https://doi.org/10.1016/0191-8141(89)90069-2
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Experimental folding and faulting of rocks under confining pressure Part IX. Wrench faults in limestone layersPublished by Elsevier ,2003
- Fault geometries in basement-induced wrench faulting under different initial stress statesPublished by Elsevier ,2003
- Strike-slip duplexesPublished by Elsevier ,2003
- TranspressionPublished by Elsevier ,2003
- Bridge structures as sense of displacement criteria in brittle fault zonesJournal of Structural Geology, 1987
- Fault-zone reactivation: kinematics and mechanismsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1986
- Origin, damping, and pattern of development of faults in graniteTectonics, 1985
- Cretaceous tectonics off mid-Norway: implications for the Rockall and Faeroe-Shetland troughsJournal of the Geological Society, 1984
- Tectonostratigraphic development of the Trondheim region Caledonides, Central NorwayJournal of Structural Geology, 1981
- The Permo-Carboniferous dyke-swarm of northern Argyll and its bearing on dextral displacement on the Great Glen FaultJournal of the Geological Society, 1979