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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Bibliographic Details
Main Authors: Thomson,William H, Garmany,Jan D, Lewis,Brian T R
Other Authors: WASHINGTON UNIV SEATTLE
Format: Text
Language:English
Published: 1980
Subjects:
Geology
Geochemistry and Mineralogy
Seismology
*Seismic waves
Iceland
Explosions
Primary waves(Seismic waves)
Secondary waves
Refraction
Earth crust
Velocity
Profiles
Online Access:http://www.dtic.mil/docs/citations/ADA115205
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA115205
Description
Summary: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.

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