dor_id: 4141299

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

561.#.#.u: https://www.geofisica.unam.mx/

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

590.#.#.b: Concentrador

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

883.#.#.a: Revistas UNAM

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

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

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

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

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1572/1694

100.1.#.a: Lieber, Paul; Wen, Kwan-sun

524.#.#.a: Lieber, Paul, et al. (1974). A primary tectonic and seismic motivating force: discovery and verification. Geofísica Internacional; Vol. 14 Núm. 1: Enero 1, 1974; 83-84. Recuperado de https://repositorio.unam.mx/contenidos/4141299

245.1.0.a: A primary tectonic and seismic motivating force: discovery and verification

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1974

264.#.1.c: 1974-01-01

653.#.#.a: Sismicidad; Tectónica; Evolución mecánica; Tierra; Summaries; Seismicity; Tectonics; Mechanical evolution; Earth

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/1572

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1572

041.#.7.h: spa

520.3.#.a: This paper presents the theoretical background which in 1965 led the senior author to the conception of a primary tectonic. motivating force and numerical results that portray its action in particular models which depict the mechanical constitution of the earth in various orders of nonuniformity. These numerical results consistently conform with the stresses which both in configuration and magnitude are necessary to account for the seismicity of certain known seismically active regions of.the earth. This primary motivating force is linked with the mechanical evolution of the earth and evidently is the primary motivator of essentially all mechanical phenomena produced in the earth. The conditions on the mechanical constitution of the earth necessary to produce this force and to sustain it in geological time are essentially equivalent to the conditions which were logically inferred in 1951* from a phenomenological description of the seismic process, namely that the earth must necessarily be:1. nonuniform in mechanical constitution2. inelastic3. at least partially maxwellian-inelastic.

773.1.#.t: Geofísica Internacional; Vol. 14 Núm. 1: Enero 1, 1974; 83-84

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: 83-84

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

doi: https://doi.org/10.22201/igeof.2954436xe.1974.14.1.1572

handle: 00b05c74318981d2

harvesting_date: 2023-06-20 17:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2023-01-16 12:26:59.0

file_modification_date: 2023-02-14 18:10:10.0

file_creator: Paul Lieber

file_name: 78e87b1730b1f60301f3f8afc75a5af39f0692f4f9700e318f21083bfbfe3372.pdf

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245.1.0.b: A primary tectonic and seismic motivating force: discovery and verification

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

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Artículo

A primary tectonic and seismic motivating force: discovery and verification

Lieber, Paul; Wen, Kwan-sun

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

Lieber, Paul, et al. (1974). A primary tectonic and seismic motivating force: discovery and verification. Geofísica Internacional; Vol. 14 Núm. 1: Enero 1, 1974; 83-84. Recuperado de https://repositorio.unam.mx/contenidos/4141299

Descripción del recurso

Autor(es)
Lieber, Paul; Wen, Kwan-sun
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
A primary tectonic and seismic motivating force: discovery and verification
Fecha
1974-01-01
Resumen
This paper presents the theoretical background which in 1965 led the senior author to the conception of a primary tectonic. motivating force and numerical results that portray its action in particular models which depict the mechanical constitution of the earth in various orders of nonuniformity. These numerical results consistently conform with the stresses which both in configuration and magnitude are necessary to account for the seismicity of certain known seismically active regions of.the earth. This primary motivating force is linked with the mechanical evolution of the earth and evidently is the primary motivator of essentially all mechanical phenomena produced in the earth. The conditions on the mechanical constitution of the earth necessary to produce this force and to sustain it in geological time are essentially equivalent to the conditions which were logically inferred in 1951* from a phenomenological description of the seismic process, namely that the earth must necessarily be:1. nonuniform in mechanical constitution2. inelastic3. at least partially maxwellian-inelastic.
Tema
Sismicidad; Tectónica; Evolución mecánica; Tierra; Summaries; Seismicity; Tectonics; Mechanical evolution; Earth
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces