Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data

Structural features of volcanic and hydrothermal systems can be used to infer the location of magma chambers or productive geothermal areas. The Hengill volcanic triple-junction complex has a well-developed geothermal system, which is being exploited to extract hot fluids that are used for electrica...

Full description

Bibliographic Details
Main Authors: Jousset, Philippe, Haberland, Christian, Bauer, Klaus, Arnasson, Knutur
Format: Report
Language:English
Published: Zenodo 2008
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.1257317
https://zenodo.org/record/1257317
_version_ 1821555930601357312
author Jousset, Philippe
Haberland, Christian
Bauer, Klaus
Arnasson, Knutur
author_facet Jousset, Philippe
Haberland, Christian
Bauer, Klaus
Arnasson, Knutur
author_sort Jousset, Philippe
collection DataCite
description Structural features of volcanic and hydrothermal systems can be used to infer the location of magma chambers or productive geothermal areas. The Hengill volcanic triple-junction complex has a well-developed geothermal system, which is being exploited to extract hot fluids that are used for electrical power and heat production. In the framework of the I-GET project, a 4-month temporary seismological network including seven high-dynamic broadband instruments was deployed and 1D transient electromagnetic soundings (TEM) and 3D magnetotelluric (MT) surveys were performed to improve the understanding of the relationships between structural features, seismic activity and fluid production at the Hengill geothermal system. The MT and TEM data set are analysed elsewhere. The analysis of the seismological data set allowed the detection and classification of more than 600 earthquakes, among which long-period (LP) earthquakes were observed for the first time in this area. This work focuses first on a joint inversion for the 3D velocity structure and determination of the locations of the hypocentres from about 250 local volcano-tectonic earthquakes with clear P- and S-wave arrival times. The results confirm those from earlier tomography studies in this area. Integrating the seismic velocity and resistivity models in a semi-quantitative approach by cross-plotting the resistivity model with the velocity ratio V P / V S delineates a structural body with a high seismic velocity ratio and low resistivity that is interpreted as the main heat source of the geothermal system. : ENGINE - FP6
format Report
genre Iceland
genre_facet Iceland
geographic Hengill
geographic_facet Hengill
id ftdatacite:10.5281/zenodo.1257317
institution Open Polar
language English
long_lat ENVELOPE(-21.306,-21.306,64.078,64.078)
op_collection_id ftdatacite
op_doi https://doi.org/10.5281/zenodo.1257317
https://doi.org/10.5281/zenodo.1257318
op_relation https://dx.doi.org/10.5281/zenodo.1257318
op_rights Open Access
info:eu-repo/semantics/openAccess
publishDate 2008
publisher Zenodo
record_format openpolar
spelling ftdatacite:10.5281/zenodo.1257317 2025-01-16T22:39:14+00:00 Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data Jousset, Philippe Haberland, Christian Bauer, Klaus Arnasson, Knutur 2008 https://dx.doi.org/10.5281/zenodo.1257317 https://zenodo.org/record/1257317 en eng Zenodo https://dx.doi.org/10.5281/zenodo.1257318 Open Access info:eu-repo/semantics/openAccess geothermal energy exploration geophysics broadband seismology Text Working paper article-journal ScholarlyArticle 2008 ftdatacite https://doi.org/10.5281/zenodo.1257317 https://doi.org/10.5281/zenodo.1257318 2021-11-05T12:55:41Z Structural features of volcanic and hydrothermal systems can be used to infer the location of magma chambers or productive geothermal areas. The Hengill volcanic triple-junction complex has a well-developed geothermal system, which is being exploited to extract hot fluids that are used for electrical power and heat production. In the framework of the I-GET project, a 4-month temporary seismological network including seven high-dynamic broadband instruments was deployed and 1D transient electromagnetic soundings (TEM) and 3D magnetotelluric (MT) surveys were performed to improve the understanding of the relationships between structural features, seismic activity and fluid production at the Hengill geothermal system. The MT and TEM data set are analysed elsewhere. The analysis of the seismological data set allowed the detection and classification of more than 600 earthquakes, among which long-period (LP) earthquakes were observed for the first time in this area. This work focuses first on a joint inversion for the 3D velocity structure and determination of the locations of the hypocentres from about 250 local volcano-tectonic earthquakes with clear P- and S-wave arrival times. The results confirm those from earlier tomography studies in this area. Integrating the seismic velocity and resistivity models in a semi-quantitative approach by cross-plotting the resistivity model with the velocity ratio V P / V S delineates a structural body with a high seismic velocity ratio and low resistivity that is interpreted as the main heat source of the geothermal system. : ENGINE - FP6 Report Iceland DataCite Hengill ENVELOPE(-21.306,-21.306,64.078,64.078)
spellingShingle geothermal energy
exploration
geophysics
broadband seismology
Jousset, Philippe
Haberland, Christian
Bauer, Klaus
Arnasson, Knutur
Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data
title Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data
title_full Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data
title_fullStr Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data
title_full_unstemmed Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data
title_short Detailled Structure Of The Hengill Geothermal Volcanic Complex, Iceland Inferred From 3-D Tomography Of High-Dynamic Broadband Seismological Data
title_sort detailled structure of the hengill geothermal volcanic complex, iceland inferred from 3-d tomography of high-dynamic broadband seismological data
topic geothermal energy
exploration
geophysics
broadband seismology
topic_facet geothermal energy
exploration
geophysics
broadband seismology
url https://dx.doi.org/10.5281/zenodo.1257317
https://zenodo.org/record/1257317