Tectonic analysis of an oceanic transform fault zone based on fault-slip data and earthquake focal mechanisms: the Husavik-Flatey Fault zone, Iceland

The Husavik-Flatey Fault (TIFF) is an oblique dextral transform fault, part of the Tjornes Fracture Zone (TFZ), that connects the North Volcanic Zone of Iceland and the Kolbeinsey Ridge. We carry out stress inversion to reconstruct the paleostress fields and present-day stress fields along the Husavik-Flatey Fault, analysing 2700 brittle tectonic data measured on the field and about 700 earthquake focal mechanisms calculated by the Icelandic Meteorological Office. This allows us to discuss the Latest Cenozoic finite deformations (from the tectonic data) as well as the present-day deformations (from the earthquake mechanisms). In both these cases, different tectonic groups are reconstructed and each of them includes several distinct stress states characterised by normal or strike-slip faulting. The stress states of a same tectonic group are related through stress permutations (sigma(1)-sigma(2) and sigma(2)-sigma(3) permutations as well as sigma(1)-sigma(3) reversals). They do not reflect separate tectonic episodes. The tectonic groups derived from the geological data and the earthquake data have striking similarity and are considered to be related. The obliquity of the Husavik-Flatey Fault implies geometric accommodation in the transform zone, resulting mainly from a dextral transtension along an ENE-WSW trend. This overall mechanism is subject to slip partitioning into two stress states: a Husavik-Flatey Fault-perpendicular, NE-SW trending extension and a Husavik-Flatey Fault-parallel, NW-SE trending extension. These three regimes occur in various local tectonic successions and not as a regional definite succession of tectonic events. The largest magnitude earthquakes reveal a regional stress field tightly related to the transform motion, whereas the lowest magnitude earthquakes depend on the local stress Fields. The field data also reveal an early extension trending similar to the spreading vector. The focal mechanism data do not reflect this extension, which occurred earlier in the evolution of the HFF and is interpreted as a stage of structural development dominated by the rifting process. (C) 2002 Elsevier Science B.V. All rights reserved.