Seismic Propagation in the Kuriles/Kamchatka Region

An analysis of seismic propagation in the crust and upper mantle of the Kuriles/Kamchatka region has been completed in support of the MSS site evaluation. Both three-dimensional ray tracing techniques and generalized ray theory methods have been utilized to model the propagation through a highly com...

Full description

Bibliographic Details
Main Authors: Hart, R. S., Kaufman, S. K.
Other Authors: SIERRA GEOPHYSICS INC ARCADIA CA
Format: Text
Language:English
Published: 1980
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA088671
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA088671
id ftdtic:ADA088671
record_format openpolar
spelling ftdtic:ADA088671 2023-05-15T16:58:39+02:00 Seismic Propagation in the Kuriles/Kamchatka Region Hart, R. S. Kaufman, S. K. SIERRA GEOPHYSICS INC ARCADIA CA 1980-07-25 text/html http://www.dtic.mil/docs/citations/ADA088671 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA088671 en eng http://www.dtic.mil/docs/citations/ADA088671 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Seismology *SEISMIC WAVES VELOCITY PROPAGATION PROFILES EARTH CRUST RAY TRACING EARTH MANTLE PACIFIC OCEAN ISLANDS LITHOSPHERE KAMCHATKA PENINSULA LITHOSPHERIC SLABS KURILE ISLANDS Text 1980 ftdtic 2016-02-20T07:40:18Z An analysis of seismic propagation in the crust and upper mantle of the Kuriles/Kamchatka region has been completed in support of the MSS site evaluation. Both three-dimensional ray tracing techniques and generalized ray theory methods have been utilized to model the propagation through a highly complex, laterally varying structure. The structural model of the upper mantle and descending lithospheric slab developed by Veith (1974) was modified for this study to include the observed change in angle of descent of the slab along the trench. The intensity of incident seismic energy at the surface was mapped and contoured for seismic rays refracting through the three-dimensional mantle structure. Synthetic seismogram profiles were also computed to investigate the waveguide effects of the lithosphere at the surface and to analyze the contribution of diffracted and multiple reflected energy, particularly within areas of classical shadow zones. (Author) Original contains color plates: All DTIC/NTIS reproductions will be in black and white. Includes transparency. Text Kamchatka Kamchatka Peninsula Defense Technical Information Center: DTIC Technical Reports database Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Seismology
*SEISMIC WAVES
VELOCITY
PROPAGATION
PROFILES
EARTH CRUST
RAY TRACING
EARTH MANTLE
PACIFIC OCEAN ISLANDS
LITHOSPHERE
KAMCHATKA PENINSULA
LITHOSPHERIC SLABS
KURILE ISLANDS
spellingShingle Seismology
*SEISMIC WAVES
VELOCITY
PROPAGATION
PROFILES
EARTH CRUST
RAY TRACING
EARTH MANTLE
PACIFIC OCEAN ISLANDS
LITHOSPHERE
KAMCHATKA PENINSULA
LITHOSPHERIC SLABS
KURILE ISLANDS
Hart, R. S.
Kaufman, S. K.
Seismic Propagation in the Kuriles/Kamchatka Region
topic_facet Seismology
*SEISMIC WAVES
VELOCITY
PROPAGATION
PROFILES
EARTH CRUST
RAY TRACING
EARTH MANTLE
PACIFIC OCEAN ISLANDS
LITHOSPHERE
KAMCHATKA PENINSULA
LITHOSPHERIC SLABS
KURILE ISLANDS
description An analysis of seismic propagation in the crust and upper mantle of the Kuriles/Kamchatka region has been completed in support of the MSS site evaluation. Both three-dimensional ray tracing techniques and generalized ray theory methods have been utilized to model the propagation through a highly complex, laterally varying structure. The structural model of the upper mantle and descending lithospheric slab developed by Veith (1974) was modified for this study to include the observed change in angle of descent of the slab along the trench. The intensity of incident seismic energy at the surface was mapped and contoured for seismic rays refracting through the three-dimensional mantle structure. Synthetic seismogram profiles were also computed to investigate the waveguide effects of the lithosphere at the surface and to analyze the contribution of diffracted and multiple reflected energy, particularly within areas of classical shadow zones. (Author) Original contains color plates: All DTIC/NTIS reproductions will be in black and white. Includes transparency.
author2 SIERRA GEOPHYSICS INC ARCADIA CA
format Text
author Hart, R. S.
Kaufman, S. K.
author_facet Hart, R. S.
Kaufman, S. K.
author_sort Hart, R. S.
title Seismic Propagation in the Kuriles/Kamchatka Region
title_short Seismic Propagation in the Kuriles/Kamchatka Region
title_full Seismic Propagation in the Kuriles/Kamchatka Region
title_fullStr Seismic Propagation in the Kuriles/Kamchatka Region
title_full_unstemmed Seismic Propagation in the Kuriles/Kamchatka Region
title_sort seismic propagation in the kuriles/kamchatka region
publishDate 1980
url http://www.dtic.mil/docs/citations/ADA088671
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA088671
long_lat ENVELOPE(160.000,160.000,56.000,56.000)
geographic Kamchatka Peninsula
Pacific
geographic_facet Kamchatka Peninsula
Pacific
genre Kamchatka
Kamchatka Peninsula
genre_facet Kamchatka
Kamchatka Peninsula
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA088671
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766050722156118016