Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey
A seismic refraction survey was conducted at Reydarfjordur, Iceland as part of the Iceland Research Drilling Project in July, 1978. An array of 15 seismometers was used to measure apparent velocities from 25 explosions along a 23 km refraction line. The experiment yielded data used to determine the...
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ftdtic:ADA115205 2023-05-15T16:46:04+02:00 Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey Thomson,William H Garmany,Jan D Lewis,Brian T R WASHINGTON UNIV SEATTLE 1980-01 text/html http://www.dtic.mil/docs/citations/ADA115205 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA115205 en eng http://www.dtic.mil/docs/citations/ADA115205 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy Seismology *Seismic waves Iceland Explosions Primary waves(Seismic waves) Secondary waves Refraction Earth crust Velocity Profiles Text 1980 ftdtic 2016-02-19T08:02:59Z A seismic refraction survey was conducted at Reydarfjordur, Iceland as part of the Iceland Research Drilling Project in July, 1978. An array of 15 seismometers was used to measure apparent velocities from 25 explosions along a 23 km refraction line. The experiment yielded data used to determine the P and S-wave vellocity structures beneath the drill site and to obtain bounds on the depth to seismic 'layer 3'. The observed apparent velocities vary continuously as a function of range with a marked increased in velocity at a range of 16 km. This corresponds to an observed cross-over in the travel time data. The measurement of apparent velocities has yielded data of the form X(p), the distance to a measured ray parameter, and alpha(p), the delay time. Joint inversion of the X(p) and alpha)p) data has been performed by linear programming. Layers of constant slowness gradient are used as the basis for the inversion process. Estimates of error in the data are used to produce extremal bounds on the family of earth models that satisfy the data. The resulting envelope of P-wave velocity models indicates a continuous variation of velocity with depth. Two regions of high velocity gradient are observed, one near the surface and the other at depths between 2.6 and 3.9 km associated with 'layer 3' in Iceland. These results suggest that modeling of Iceland's upper crust with a few thick homogeneous constant velocity layers is an inadequate representation of the velocity structure. Text Iceland Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Geology Geochemistry and Mineralogy Seismology *Seismic waves Iceland Explosions Primary waves(Seismic waves) Secondary waves Refraction Earth crust Velocity Profiles |
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Geology Geochemistry and Mineralogy Seismology *Seismic waves Iceland Explosions Primary waves(Seismic waves) Secondary waves Refraction Earth crust Velocity Profiles Thomson,William H Garmany,Jan D Lewis,Brian T R Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey |
topic_facet |
Geology Geochemistry and Mineralogy Seismology *Seismic waves Iceland Explosions Primary waves(Seismic waves) Secondary waves Refraction Earth crust Velocity Profiles |
description |
A seismic refraction survey was conducted at Reydarfjordur, Iceland as part of the Iceland Research Drilling Project in July, 1978. An array of 15 seismometers was used to measure apparent velocities from 25 explosions along a 23 km refraction line. The experiment yielded data used to determine the P and S-wave vellocity structures beneath the drill site and to obtain bounds on the depth to seismic 'layer 3'. The observed apparent velocities vary continuously as a function of range with a marked increased in velocity at a range of 16 km. This corresponds to an observed cross-over in the travel time data. The measurement of apparent velocities has yielded data of the form X(p), the distance to a measured ray parameter, and alpha(p), the delay time. Joint inversion of the X(p) and alpha)p) data has been performed by linear programming. Layers of constant slowness gradient are used as the basis for the inversion process. Estimates of error in the data are used to produce extremal bounds on the family of earth models that satisfy the data. The resulting envelope of P-wave velocity models indicates a continuous variation of velocity with depth. Two regions of high velocity gradient are observed, one near the surface and the other at depths between 2.6 and 3.9 km associated with 'layer 3' in Iceland. These results suggest that modeling of Iceland's upper crust with a few thick homogeneous constant velocity layers is an inadequate representation of the velocity structure. |
author2 |
WASHINGTON UNIV SEATTLE |
format |
Text |
author |
Thomson,William H Garmany,Jan D Lewis,Brian T R |
author_facet |
Thomson,William H Garmany,Jan D Lewis,Brian T R |
author_sort |
Thomson,William H |
title |
Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey |
title_short |
Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey |
title_full |
Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey |
title_fullStr |
Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey |
title_full_unstemmed |
Crustal Structure Near the Iceland Research Drilling Project Borehole from a Seismic Refraction Survey |
title_sort |
crustal structure near the iceland research drilling project borehole from a seismic refraction survey |
publishDate |
1980 |
url |
http://www.dtic.mil/docs/citations/ADA115205 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA115205 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA115205 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766036197438652416 |