Vista normal Vista MARC

Tectonics and the formation of magmas [Libro electrónico] / Yu. M. Sheinmann

Por: Sheinmann, Yu. M [autor/a].
Tipo de material: Libro en línea Libro en línea Editor: New York, New York, United States: Consultants Bureau, c1971Descripción: x, 173 páginas : ilustraciones mapas ; 28 centímetros.ISBN: 0306108593; 9781468415865 (Print); 9781468415841 (Online).Tema(s): Geology, Structural | Igneous rocks | Earth movementsNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía: páginas 167-173 Número de sistema: 55473Contenidos:Mostrar Resumen:
Inglés

It is a pleasure to any author to enlarge the circle of his readers. Naturally this is a pleasure to me. At the same time, however, misgivings arise: whether these pages will con­ vey to the circle of new readers the thoughts that excite the author. Science is advancing rapidly in our day. It is already apparent that many things in the book should have been stated differently. I have tried to make additions to the English-language edition in such a way that they do not require great alteration of the text. I ask my new readers to remember that this book was written primarily for my fellow countrymen and that, because of this, some chapters contain descriptions of regions little known to you and information on the USSR almost unknown from other publications. I hope that, despite this, geologists who read the English-language edition will find something of interest to themselves in it and that their labor will not have been in vain. Yu. M. Sheinmann Institute of Phys ics of the Earth Moscow v PREFACE The study of endogenetic processes has long pushed us into investigation of ever deeper parts of the earth. Not long ago all attention was focused on depths where ore deposits appear, where metamorphic and igneous rocks, which later become exposed at the surface, are formed, where granites originate.

Recurso en línea: http://link.springer.com/openurl?genre=book&isbn=978-1-4684-1586-5
Etiquetas de esta biblioteca: No hay etiquetas de esta biblioteca para este título. Ingresar para agregar etiquetas.
Star ratings
    Valoración media: 0.0 (0 votos)
Existencias
Tipo de ítem Biblioteca actual Colección Signatura Estado Fecha de vencimiento Código de barras
Libros Biblioteca Electrónica
Recursos en línea (RE) 		Acervo General Recurso digital ECO400554736070

Incluye bibliografía: páginas 167-173

1. Introduction.. 2. What prevents direct comparison of petrologic and tectonic data?.. 3. The possibility of understanding the tectonics of deep-seated regions and a method proposed for studying it.. 4. Regional tectonic subdivisions according to depth.. 5. Orientation of stresses and the geometry of deep-focus earthquakes.. 6. Primary magmas.. 7. The tectonic distribution of primary magmas.. 8. The extrageosynclinal type of magmatic development.. 9. Magmatic features of midocean ridges.. 10. Geosynclinal magmas.. 11. Silicic magmas (magma formation in the crust.. 12. Volcanic (volcanic-plutonic belts.. 13. Magma and the subsidence of ocean basins (concerning "oceanization".. 14. Conditions for the appearance of magma.. 15. Conclusions.. Bibliography

Disponible para usuarios de ECOSUR con su clave de acceso

It is a pleasure to any author to enlarge the circle of his readers. Naturally this is a pleasure to me. At the same time, however, misgivings arise: whether these pages will con­ vey to the circle of new readers the thoughts that excite the author. Science is advancing rapidly in our day. It is already apparent that many things in the book should have been stated differently. I have tried to make additions to the English-language edition in such a way that they do not require great alteration of the text. I ask my new readers to remember that this book was written primarily for my fellow countrymen and that, because of this, some chapters contain descriptions of regions little known to you and information on the USSR almost unknown from other publications. I hope that, despite this, geologists who read the English-language edition will find something of interest to themselves in it and that their labor will not have been in vain. Yu. M. Sheinmann Institute of Phys ics of the Earth Moscow v PREFACE The study of endogenetic processes has long pushed us into investigation of ever deeper parts of the earth. Not long ago all attention was focused on depths where ore deposits appear, where metamorphic and igneous rocks, which later become exposed at the surface, are formed, where granites originate. eng

Disponible en línea

Disponible en formato PDF

Subscripción a ELSEVIER 26 de diciembre del 2013

Con tecnología Koha