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Geology; August 2004; v. 32; no. 8; p. 641-644; DOI: 10.1130/G20542.1
© 2004 Geological Society of America
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Hydrogeochemical changes before and after a major earthquake

Lillemor Claesson1, Alasdair Skelton*,2, Colin Graham*,3, Carlo Dietl*,4, Magnus Mörth*,6, Peter Torssander*,6 and Ingrid Kockum*,7

1 Department of Geology and Geochemistry, Stockholm University, 106 91 Stockholm, Sweden, and Nordic Volcanological Institute, ASKJA, Sturlugata 7, IS-101 Reykjavik, Iceland
2 Department of Geology and Geochemistry, Stockholm University, 106 91 Stockholm, Sweden
3 School of Geosciences, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, Scotland
4 Geologisches Institut, Julius-Maximilians-Universität, Pleicherwall 1, 97070 Würzburg, Germany
6 Department of Geology and Geochemistry, Stockholm University, 106 91 Stockholm, Sweden
7 Department of Molecular Medicine, Karolinska Institutet, 171 76 Stockholm, Sweden

Hydrogeochemical changes were detected by monitoring ice age meteoric waters before and after a magnitude (M) 5.8 earthquake on 16 September 2002 in the Tjörnes Fracture Zone, northern Iceland. Significant Cu, Zn, Mn, and Cr anomalies reached our sampling station 1, 2, 5, and ≥10 weeks before the earthquake, respectively. By comparison with published experimental, geophysical, and geochemical studies, we suggest stress-induced source mixing and leakage of fluid from an external (hotter) basalt-hosted source reservoir, where fluid-rock interaction was more rapid. Rapid 12%–19% increases in the concentrations of B, Ca, K, Li, Mo, Na, Rb, S, Si, Sr, Cl, and SO4, and decreases in Na/Ca, {delta}18O, and {delta}D, occurred 2–9 days after the earthquake. The rapidity of these changes is consistent with time scales of fault sealing due to coupled deformation and fluid flow. We interpret fluid-source switching in response to fault sealing and unsealing, with the newly tapped aquifer containing chemically and isotopically distinct ice age meteoric water. Variation in Na/Ca ratio appears to be sensitive to the changing stress state associated with M > 4 earthquakes. This study highlights the potential of hydrogeochemical change in earthquake-prediction studies.

Key Words: hydrogeochemistry • earthquake prediction • source mixing • source switching • ice age meteoric water • Iceland







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