Detailed Oceanic Crustal Modeling.
The research performed under this contract can be divided into 3 main topics: changes in existing methods, Cagniard de-Hoop and WKBJ, which enable construction of synthetics for mixed path simulations; use of long period SH waves with source in the Northwest Atlantic and receivers on the northeast c...
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ftdtic:ADA148589 2023-05-15T17:34:03+02:00 Detailed Oceanic Crustal Modeling. Helmberger,D V CALIFORNIA INST OF TECH PASADENA SEISMOLOGICAL LAB 1984-11-07 text/html http://www.dtic.mil/docs/citations/ADA148589 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA148589 en eng http://www.dtic.mil/docs/citations/ADA148589 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Numerical Mathematics Acoustics *OCEAN WAVES *OCEAN MODELS *OCEANIC CRUST SHEAR PROPERTIES SIMULATION COASTAL REGIONS MATHEMATICAL ANALYSIS SEISMIC WAVES ACOUSTIC ATTENUATION EARTHQUAKES ACOUSTIC VELOCITY NORTH ATLANTIC OCEAN STRUCTURAL GEOLOGY PRIMARY WAVES(SEISMIC WAVES) EARTH MANTLE Kirchoff Helmholtz integral equation PE083399 Text 1984 ftdtic 2016-02-20T23:34:37Z The research performed under this contract can be divided into 3 main topics: changes in existing methods, Cagniard de-Hoop and WKBJ, which enable construction of synthetics for mixed path simulations; use of long period SH waves with source in the Northwest Atlantic and receivers on the northeast coast of North America to derive an oceanic upper mantle shear velocity model; and a technique based on evaluating the Kirchoff-Helmholtz integral for predicting the effect of near source or near receiver structure complexity on far field p waves. In Section II we assess the fact that recent models of upper mantle structure based on long period body waves (WWSSN) suggest large horizontal gradients, especially in shear velocities. Some changes in existing methods are required to construct synthetics for mixed path situations. This is accomplished by allowing locally dipping structure and making some modifications to generalized ray theory. In Section III, we have modeled the SH motion from earthquakes in the northwest Atlantic ocean to derive an oceanic upper mantle shear velocity model. In Section IV, we extend the Kirchoff-Helmholtz integral method to calculate acoustic potentials which transmit through three dimensional warped boundaries. Text North Atlantic Northwest Atlantic 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 |
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ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Numerical Mathematics Acoustics *OCEAN WAVES *OCEAN MODELS *OCEANIC CRUST SHEAR PROPERTIES SIMULATION COASTAL REGIONS MATHEMATICAL ANALYSIS SEISMIC WAVES ACOUSTIC ATTENUATION EARTHQUAKES ACOUSTIC VELOCITY NORTH ATLANTIC OCEAN STRUCTURAL GEOLOGY PRIMARY WAVES(SEISMIC WAVES) EARTH MANTLE Kirchoff Helmholtz integral equation PE083399 |
spellingShingle |
Physical and Dynamic Oceanography Numerical Mathematics Acoustics *OCEAN WAVES *OCEAN MODELS *OCEANIC CRUST SHEAR PROPERTIES SIMULATION COASTAL REGIONS MATHEMATICAL ANALYSIS SEISMIC WAVES ACOUSTIC ATTENUATION EARTHQUAKES ACOUSTIC VELOCITY NORTH ATLANTIC OCEAN STRUCTURAL GEOLOGY PRIMARY WAVES(SEISMIC WAVES) EARTH MANTLE Kirchoff Helmholtz integral equation PE083399 Helmberger,D V Detailed Oceanic Crustal Modeling. |
topic_facet |
Physical and Dynamic Oceanography Numerical Mathematics Acoustics *OCEAN WAVES *OCEAN MODELS *OCEANIC CRUST SHEAR PROPERTIES SIMULATION COASTAL REGIONS MATHEMATICAL ANALYSIS SEISMIC WAVES ACOUSTIC ATTENUATION EARTHQUAKES ACOUSTIC VELOCITY NORTH ATLANTIC OCEAN STRUCTURAL GEOLOGY PRIMARY WAVES(SEISMIC WAVES) EARTH MANTLE Kirchoff Helmholtz integral equation PE083399 |
description |
The research performed under this contract can be divided into 3 main topics: changes in existing methods, Cagniard de-Hoop and WKBJ, which enable construction of synthetics for mixed path simulations; use of long period SH waves with source in the Northwest Atlantic and receivers on the northeast coast of North America to derive an oceanic upper mantle shear velocity model; and a technique based on evaluating the Kirchoff-Helmholtz integral for predicting the effect of near source or near receiver structure complexity on far field p waves. In Section II we assess the fact that recent models of upper mantle structure based on long period body waves (WWSSN) suggest large horizontal gradients, especially in shear velocities. Some changes in existing methods are required to construct synthetics for mixed path situations. This is accomplished by allowing locally dipping structure and making some modifications to generalized ray theory. In Section III, we have modeled the SH motion from earthquakes in the northwest Atlantic ocean to derive an oceanic upper mantle shear velocity model. In Section IV, we extend the Kirchoff-Helmholtz integral method to calculate acoustic potentials which transmit through three dimensional warped boundaries. |
author2 |
CALIFORNIA INST OF TECH PASADENA SEISMOLOGICAL LAB |
format |
Text |
author |
Helmberger,D V |
author_facet |
Helmberger,D V |
author_sort |
Helmberger,D V |
title |
Detailed Oceanic Crustal Modeling. |
title_short |
Detailed Oceanic Crustal Modeling. |
title_full |
Detailed Oceanic Crustal Modeling. |
title_fullStr |
Detailed Oceanic Crustal Modeling. |
title_full_unstemmed |
Detailed Oceanic Crustal Modeling. |
title_sort |
detailed oceanic crustal modeling. |
publishDate |
1984 |
url |
http://www.dtic.mil/docs/citations/ADA148589 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA148589 |
genre |
North Atlantic Northwest Atlantic |
genre_facet |
North Atlantic Northwest Atlantic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA148589 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766132740181196800 |