dor_id: 4132306

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

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883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

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850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1506/1626

100.1.#.a: Kunar, L.N.S.

524.#.#.a: Kunar, L.N.S. (1975). Bubble pulses and power spectra of some marine seismograms. Geofísica Internacional; Vol. 15 Núm. 1: Enero 1, 1975; 45-63. Recuperado de https://repositorio.unam.mx/contenidos/4132306

245.1.0.a: Bubble pulses and power spectra of some marine seismograms

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1975

264.#.1.c: 1975-01-01

653.#.#.a: Sismología; Sismogramas marinos; Oscilaciones pulsátiles de burbuja; Seismology; Marine seismograms; Bubble pulse oscillations

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1506

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1506

041.#.7.h: spa

520.3.#.a: Marine seismograms from a marine refraction survey done in Lake Superior with "geogel" explosives are studied in terms of their spectral content in relation to various shot sizes (1.25-200 lbs). The effect of bubble pulse oscillations plays a dominant role in the analysis. A heuristic approach is used throughout and it is concluded that the use of small shots is advisable, whenever possible, in marine refraction surveys on account of the relatively broad advisable, whenever possible, in marine refraction surveys on account of the relatively broad spectra in comparison with those for larger shots. Also, if a deconvolution process is used to remove the bubble pulse effects from a seismogram having a narrow spectrum, nothing very meaningful would remain for interpretation. From observations of the bubble pulse periods, sizes of shots, and depths of detonation, the Rayleigh-Willis constant is determined for the Lake Superior environment. The calculated value of 5.0 yields bubble periods comparable to those observed. However this value differs from other values such as 4.19 obtained by Worzel and Ewing (1948) and 4.36 obtained by a group at Woods Hole Oceanographic Institute (Shor, 1963) using TNT explosives at sea. The constant seems dependent on both the type of explosive and the shooting environment.

773.1.#.t: Geofísica Internacional; Vol. 15 Núm. 1: Enero 1, 1975; 45-63

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 45-63

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.1975.15.1.952

handle: 4b262473f1cac1a5

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2008-06-27 23:26:34.0

file_modification_date: 2023-02-03 13:17:07.0

file_creator: L.N. S. Kunar

file_name: 5af5afa41140ed5f18960847ff7808115656e2802e906a5b063be37608253faf.pdf

file_pages_number: 19

file_format_version: application/pdf; version=1.6

file_size: 4580712

245.1.0.b: Bubble pulses and power spectra of some marine seismograms

last_modified: 2023-06-20 16:00:00

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

license_type: by-nc-sa

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Artículo

Bubble pulses and power spectra of some marine seismograms

Kunar, L.N.S.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Kunar, L.N.S. (1975). Bubble pulses and power spectra of some marine seismograms. Geofísica Internacional; Vol. 15 Núm. 1: Enero 1, 1975; 45-63. Recuperado de https://repositorio.unam.mx/contenidos/4132306

Descripción del recurso

Autor(es)
Kunar, L.N.S.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Bubble pulses and power spectra of some marine seismograms
Fecha
1975-01-01
Resumen
Marine seismograms from a marine refraction survey done in Lake Superior with "geogel" explosives are studied in terms of their spectral content in relation to various shot sizes (1.25-200 lbs). The effect of bubble pulse oscillations plays a dominant role in the analysis. A heuristic approach is used throughout and it is concluded that the use of small shots is advisable, whenever possible, in marine refraction surveys on account of the relatively broad advisable, whenever possible, in marine refraction surveys on account of the relatively broad spectra in comparison with those for larger shots. Also, if a deconvolution process is used to remove the bubble pulse effects from a seismogram having a narrow spectrum, nothing very meaningful would remain for interpretation. From observations of the bubble pulse periods, sizes of shots, and depths of detonation, the Rayleigh-Willis constant is determined for the Lake Superior environment. The calculated value of 5.0 yields bubble periods comparable to those observed. However this value differs from other values such as 4.19 obtained by Worzel and Ewing (1948) and 4.36 obtained by a group at Woods Hole Oceanographic Institute (Shor, 1963) using TNT explosives at sea. The constant seems dependent on both the type of explosive and the shooting environment.
Tema
Sismología; Sismogramas marinos; Oscilaciones pulsátiles de burbuja; Seismology; Marine seismograms; Bubble pulse oscillations
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces