Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area

Volcanic rifting environments, such as in Iceland, are challenging for conventional seismic reflection methods using active surface seismic sources. This study demonstrates the potential of a novel technique, called Virtual Reflection Seismic Profiling (VRSP) for imaging reflections in geothermal re...

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Main Author: Stoch, Agnieszka
Format: Others
Language:English
Published: Uppsala universitet, Geofysik 2020
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-413199
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spelling ndltd-UPSALLA1-oai-DiVA.org-uu-4131992020-07-22T05:48:24ZAnalysis of Seismic Data Acquired in the Hverahlíð Geothermal AreaengStoch, AgnieszkaUppsala universitet, Geofysik2020Hverahlíð geothermal areareflection seismicvirtual reflection seismic profilingvirtual shot gathercross-correlationautocorrelationGeophysicsGeofysikVolcanic rifting environments, such as in Iceland, are challenging for conventional seismic reflection methods using active surface seismic sources. This study demonstrates the potential of a novel technique, called Virtual Reflection Seismic Profiling (VRSP) for imaging reflections in geothermal regions, like Hverahlíð, where a dense seismic array recorded a number of local microearthquakes for cross-correlation. Uppsala University, in collaboration with Reykjavik Energy, recorded seismicity in Hverahlíð using both seismometers and geophones. Acquired data were processed using the VRSP method, which applies seismic interferometry only to selected events, in this thesis local microearthquakes. Cross-correlation of the signal from a microearthquake recorded at one of the stations, which acts as a virtual source, with a ghost reflection recorded by the remaining receivers, produces a virtual shot gather. Stacking each station’s result, for all available events, and following a conventional multichannel processing sequence resulted in two stacked seismic images. Potential reflections observed in the obtained sections could be associated with major feed zones identified in the area by the borehole measurements. Eight dynamite explosions were processed with a conventional seismic reflection method, as a complementary source to the microearthquakes. In the produced stacked seismic section two potential reflections could be observed. Results from both passive and active datasets were 3D visualised to verify whether the reflections correspond to each other between sections. Two horizons were traced throughout all three stacked sections. One more interface appeared on two images obtained from processing the passive data. This study shows promising results for using natural sources to image the subsurface in a challenging environment. Student thesisinfo:eu-repo/semantics/bachelorThesistexthttp://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-413199Examensarbete vid Institutionen för geovetenskaper, 1650-6553 ; 485application/pdfinfo:eu-repo/semantics/openAccess
collection NDLTD
language English
format Others
sources NDLTD
topic Hverahlíð geothermal area
reflection seismic
virtual reflection seismic profiling
virtual shot gather
cross-correlation
autocorrelation
Geophysics
Geofysik
spellingShingle Hverahlíð geothermal area
reflection seismic
virtual reflection seismic profiling
virtual shot gather
cross-correlation
autocorrelation
Geophysics
Geofysik
Stoch, Agnieszka
Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area
description Volcanic rifting environments, such as in Iceland, are challenging for conventional seismic reflection methods using active surface seismic sources. This study demonstrates the potential of a novel technique, called Virtual Reflection Seismic Profiling (VRSP) for imaging reflections in geothermal regions, like Hverahlíð, where a dense seismic array recorded a number of local microearthquakes for cross-correlation. Uppsala University, in collaboration with Reykjavik Energy, recorded seismicity in Hverahlíð using both seismometers and geophones. Acquired data were processed using the VRSP method, which applies seismic interferometry only to selected events, in this thesis local microearthquakes. Cross-correlation of the signal from a microearthquake recorded at one of the stations, which acts as a virtual source, with a ghost reflection recorded by the remaining receivers, produces a virtual shot gather. Stacking each station’s result, for all available events, and following a conventional multichannel processing sequence resulted in two stacked seismic images. Potential reflections observed in the obtained sections could be associated with major feed zones identified in the area by the borehole measurements. Eight dynamite explosions were processed with a conventional seismic reflection method, as a complementary source to the microearthquakes. In the produced stacked seismic section two potential reflections could be observed. Results from both passive and active datasets were 3D visualised to verify whether the reflections correspond to each other between sections. Two horizons were traced throughout all three stacked sections. One more interface appeared on two images obtained from processing the passive data. This study shows promising results for using natural sources to image the subsurface in a challenging environment.
author Stoch, Agnieszka
author_facet Stoch, Agnieszka
author_sort Stoch, Agnieszka
title Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area
title_short Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area
title_full Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area
title_fullStr Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area
title_full_unstemmed Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area
title_sort analysis of seismic data acquired in the hverahlíð geothermal area
publisher Uppsala universitet, Geofysik
publishDate 2020
url http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-413199
work_keys_str_mv AT stochagnieszka analysisofseismicdataacquiredinthehverahliðgeothermalarea
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