Effect of tectonics and earthquakes on geothermal activity near plate boundaries: A case study from South Iceland

We studied fracture-controlled geothermal fields in the Hreppar Rift-Jump Block (HRJB), a micro-plate bounded by two NNE rifts and the E-W transform zone of the South Iceland Seismic Zone (SISZ). Distinguishing whether the extensional rift swarm or the transform zone shear fractures host the geother...

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Veröffentlicht in:Geothermics 2010-09, Vol.39 (3), p.207-219
Hauptverfasser: KHODAYAR, Maryam, BJÖRNSSON, Sveinbjörn, EINARSSON, Páll, FRANZSON, Hjalti
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container_end_page 219
container_issue 3
container_start_page 207
container_title Geothermics
container_volume 39
creator KHODAYAR, Maryam
BJÖRNSSON, Sveinbjörn
EINARSSON, Páll
FRANZSON, Hjalti
description We studied fracture-controlled geothermal fields in the Hreppar Rift-Jump Block (HRJB), a micro-plate bounded by two NNE rifts and the E-W transform zone of the South Iceland Seismic Zone (SISZ). Distinguishing whether the extensional rift swarm or the transform zone shear fractures host the geothermal activity is challenging. GPS mapping of 208 springs and tectonic analysis indicate that six Riedel shear fracture sets of an older transform zone in the HRJB are permeable. Northerly dextral strike-slip faults are the principal permeable faults, although the highest discharge and temperature are found at their intersections with other fracture sets. Two northerly faults from the HRJB connect to the source faults of the major 1784 and 1896 earthquakes within the active SISZ. The 1784 earthquake caused pressure changes as far north as the studied springs, indicating that earthquakes keep faults permeable over hundreds of years.
doi_str_mv 10.1016/j.geothermics.2010.06.003
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subjects Earth sciences
Earth, ocean, space
Earthquakes
Engineering and environment geology. Geothermics
Exact sciences and technology
Faults
Fracture mechanics
Geothermal
Geothermics
Global Positioning System
Satellite navigation systems
Seismic phenomena
Transforms
title Effect of tectonics and earthquakes on geothermal activity near plate boundaries: A case study from South Iceland
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