dor_id: 41852

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

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336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1141/1119

100.1.#.a: Tozer, Davidc

524.#.#.a: Tozer, Davidc. (1973). The concept of a lithosphere. Geofísica Internacional; Vol. 13 No. 4, 1973. Recuperado de https://repositorio.unam.mx/contenidos/41852

245.1.0.a: The concept of a lithosphere

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1973

264.#.1.c: 2013-01-21

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-ND 4.0 Internacional, https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode.es, fecha de asignación de la licencia 2013-01-21, para un uso diferente consultar al responsable jurídico del repositorio por medio de revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1141

001.#.#.#: oai:ojs.ojs.geofisica.unam.mx:article/1141

041.#.7.h: spa

520.3.#.a: The current tendency to define a lithosphere as an elastically distinct region is in danger of distorting an important qualitative insight into the tectonic processes of a planet. Just as we recognize on a laboratory scale that a given material can believe quasi elastically (solid-like) or quasi viscously (liquid-like) under different regimes of loading, it is suggested that the word lithosphere be used to describe that part of a planet, if any, that behaves quasi elastically under the stresses associated with the heat transfer process. The delimiting of such a region necessarily involves a discussion of the non elastic behaviour of planetary material. This idea is developed in particular for the Earth, although reference is made to other planets. Such a lithosphere is much thinner than one based on the ´depth of the low velocity´ and is probably several times thicker under continues than oceans. This is very relevant to the stability, and hence radiogenic age of the lothosphere in the two regions. A quite distinet explanation of the oceanic low velocity layer is offered.

773.1.#.t: Geofísica Internacional; Vol. 13 No. 4 (1973)

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

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Artículo

The concept of a lithosphere

Tozer, Davidc

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

Tozer, Davidc. (1973). The concept of a lithosphere. Geofísica Internacional; Vol. 13 No. 4, 1973. Recuperado de https://repositorio.unam.mx/contenidos/41852

Descripción del recurso

Autor(es)
Tozer, Davidc
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
The concept of a lithosphere
Fecha
2013-01-21
Resumen
The current tendency to define a lithosphere as an elastically distinct region is in danger of distorting an important qualitative insight into the tectonic processes of a planet. Just as we recognize on a laboratory scale that a given material can believe quasi elastically (solid-like) or quasi viscously (liquid-like) under different regimes of loading, it is suggested that the word lithosphere be used to describe that part of a planet, if any, that behaves quasi elastically under the stresses associated with the heat transfer process. The delimiting of such a region necessarily involves a discussion of the non elastic behaviour of planetary material. This idea is developed in particular for the Earth, although reference is made to other planets. Such a lithosphere is much thinner than one based on the ´depth of the low velocity´ and is probably several times thicker under continues than oceans. This is very relevant to the stability, and hence radiogenic age of the lothosphere in the two regions. A quite distinet explanation of the oceanic low velocity layer is offered.
Idioma
spa
ISSN
0016-7169

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