Magmatic and tectonic history of Iceland's western rift zone at Lake Thingvallavatn
Bull, J.M., Minshull, T.A., Mitchell, N.C., Dix, J.K. and Hardardottir, J. (2005) Magmatic and tectonic history of Iceland's western rift zone at Lake Thingvallavatn. Geological Society of America Bulletin, 117, (11-12), 1451-1465. (doi:10.1130/B25729.1).
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High rates of Holocene sedimentation in a lake spanning the Thingvellir rift zone of western Iceland provide an unusual opportunity to study the interaction of tectonic and magmatic processes on timescales of thousands of years. Lake Thingvallavatn is oriented SW-NE, parallel to the trend of normal faults and fissures which extend northeast from Hengill, a central volcano system. Thingvallavatn’s lake sediments provide a continuous high-fidelity record of tectono-magmatic processes. “Chirp” sub-bottom profiler and sidescan records, together with sediment core information, enabled the lake stratigraphy to be constrained well since the emplacement of a post-glacial lava at 9.1 ± 0.3 ka. This lava, together with three younger horizons, enabled detailed study of the main tectonic and magmatic events. A major Hengill volcanic event which controlled the development of the present-day lake morphology occurred at 1.9 ka with the eruption of a scoria cone within the lake (Sandey). During this event, the Nesjahraun lava was erupted into the southern part of the lake, the Sandey scoria cone was formed, and major faulting and subsidence occurred in the northern part of the lake, resulting in the formation of an asymmetrical rift. Within the southern part of the lake, a deformed sequence of sediments of age 2.9 – 1.5 ka, between undeformed younger and older sediments, indicate that liquefaction phenomena are associated with the emplacement of the Nesjahraun lava. Analysis of fault displacement reveals that the total throw summed over all faults across the width of the rift zone is approximately constant (110 - 130 m) along the long axis of the rift. We estimate an extension rate on the faults of 3.3 – 8.2 mm yr-1 since 9.1 ka, assuming fault dips of 60 - 75°, which represents 17 – 43 % of the total plate boundary extension estimated from global plate motion inversion. We speculate that the remaining extension must either be taken up elsewhere in Iceland, for example in the Eastern Rift Zone or along the South Island Seismic Zone, or that extension estimated over the last 9kyr underestimates the long-term extension rate due to incomplete sampling of the episodic magmatic component.
|Digital Object Identifier (DOI):||doi:10.1130/B25729.1|
|Keywords:||neotectonics, dikes, subsidence, normal faults, Iceland, liquefaction|
|Subjects:||Q Science > QE Geology|
|Divisions:||University Structure - Pre August 2011 > School of Ocean & Earth Science (SOC/SOES)
|Date Deposited:||09 May 2006|
|Last Modified:||11 Jan 2016 16:15|
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
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