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Triggering of microearthquakes in Iceland by volatiles released from a dyke intrusion

Martens, Hilary R. and White, Robert S. (2013) Triggering of microearthquakes in Iceland by volatiles released from a dyke intrusion. Geophysical Journal International, 194 (3). pp. 1738-1754. ISSN 0956-540X. https://resolver.caltech.edu/CaltechAUTHORS:20130920-153452453

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Abstract

We suggest that carbon dioxide exsolved from a mid-crustal basaltic dyke intrusion in Iceland migrated upwards and triggered shallow seismicity by allowing failure on pre-existing fractures under the relatively low elastic stresses (100–200 kPa; 1–2 bar) generated by the dyke inflation. Intense swarms of microseismicity accompanied magmatic intrusion into a dyke at depths of 13–19 km in the crust of Iceland's Northern Volcanic Rift Zone during 2007–2008. Contemporaneously, a series of small normal earthquakes, probably triggered by elastic stresses imposed by the dyke intrusion, occurred in the uppermost 4 km of crust: fault plane solutions from these are consistent with failure along the extensional fabric and surface fissure directions mapped in the area, suggesting that the faults failed along existing rift zone fabric even though the mid-crustal dyke is highly oblique to it. Several months after the melt froze in the mid-crust and seismicity associated with the intrusion had ceased, an upsurge in shallow microseismicity began in the updip projection of the dyke near the brittle–ductile transition at 6–7 km depth below sea level. This seismicity is caused by failure on right-lateral strike-slip faults, with fault planes orientated 23 ± 3°, which are identical with the 24 ± 2° orientation in this area of surface fractures and fissures caused by plate spreading and extension of the volcanic rift zone. However, these earthquakes have T-axes approximately aligned with the opening direction of the dyke, and the right-lateral sense of failure is opposite that of regional strike-slip faults. We suggest that the fractures occurred along pre-existing weaknesses generated by the pervasive fabric of the rift zone, but that the dyke opening in the mid-crust beneath it caused right-lateral failure. The seismicity commenced after a temporal delay of several months and has persisted for over 3 yr. We propose that fluids exsolved from the magma in the dyke, primarily carbon dioxide, percolated updip and to shallower depths predominantly along pre-existing fractures. Increased pore pressure from the volatiles reduced the effective normal compressive stress on faults, increasing the likelihood of failure and allowing the modest stress changes generated by the intrusion to cause failure. Propagation of volatiles through the crust would also account for the observed time delay between the intrusion at depth and the shallow earthquake clusters. A further short-lived cluster of earthquakes at 2–4 km depth beneath the surface exhibits left-lateral strike-slip faulting with epicentres well orientated along a lineation which is identical with other subparallel strike-slip faults in the area that transfer motion between two adjacent spreading segments. These shallow earthquakes lie beyond lobes of significant positive Coulomb stress change caused by the intrusion, implying minimal modifications to the stress field in their vicinity; hence, they continue to respond to the regional stress field rather than the local stress field generated by the dyke intrusion.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1093/gji/ggt184 DOIArticle
http://gji.oxfordjournals.org/content/194/3/1738PublisherArticle
Additional Information:© 2013 The Authors. Published by Oxford University Press on behalf of The Royal Astronomical Society. Accepted 2013 May 4. Received 2013 May 1; in original form 2013 February 7. First published online: June 3, 2013. Seismometers were borrowed from the Natural Environment Research Council SEIS-UK (loans 842 and 914). We thank Heidi Soosalu, Janet Key and all those who have assisted in fieldwork in Iceland since 2007. We are grateful to Ásta Hjartardöttir and Páll Einarsson for providing raw data on fracture orientations from the Upptyppingar region and to Rob Green for providing epicentral locations from his work on earthquakes on strike-slip faults between the Askja and Kverkfjöll segments. We thank Marie Edmonds and John Maclennan for giving valuable advice on carbon dioxide concentrations and degassing in Icelandic lavas.We acknowledge Alex Copley and Nadia Lapusta for providing helpful comments on the modelling portion of this manuscript and thank Brad Aagaard and Charles Williams for training and support in using Pylith. We also appreciate the helpful suggestions made by two anonymous reviewers to strengthen the manuscript. The IMO kindly provided data from their seismometers in northeast Iceland. This manuscript is based upon work supported by the National Science Foundation Graduate Research Fellowship to HRM under Grant No. DGE-1144469. Department of Earth Sciences, Cambridge contribution number ESC2755.
Funders:
Funding AgencyGrant Number
NSF Graduate Research FellowshipDGE-1144469
Subject Keywords:Fracture and flow; Earthquake interaction, forecasting, and prediction; Volcano seismology; Rheology and friction of fault zones; Dynamics and mechanics of faulting; Volcanic gases
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Cambridge Department of Earth SciencesESC2755
Issue or Number:3
Record Number:CaltechAUTHORS:20130920-153452453
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20130920-153452453
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:41457
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:20 Sep 2013 23:18
Last Modified:03 Oct 2019 05:49

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