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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Main Author: Helmberger,D V
Other Authors: CALIFORNIA INST OF TECH PASADENA SEISMOLOGICAL LAB
Format: Text
Language:English
Published: 1984
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA148589
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA148589
id ftdtic:ADA148589
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spelling 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
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id 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