Verlag: Programa Explora - Conicyt, Universidad Católica del Norte, 2002
ISBN 10: 9562910806 ISBN 13: 9789562910804
Anbieter: Librería Monte Sarmiento, Santiago, SANTI, Chile
Encuadernación de tapa blanda. Zustand: Bien. 2ª Edición. 158 p. + anexos ; 27x20 cm., ilustraciones en color, mapas. Glosario (BN-7)(ID-c).
Anbieter: ThriftBooks-Atlanta, AUSTELL, GA, USA
Hardcover. Zustand: Very Good. No Jacket. Former library book; May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less.
Verlag: Explora - Conicyt, Santiago de Chile, 2003
ISBN 10: 9562990079 ISBN 13: 9789562990073
Anbieter: Librería Monte Sarmiento, Santiago, SANTI, Chile
Erstausgabe
Encuadernación de tapa blanda. Zustand: Bien. 1ª Edición. 277, xi, iv p. ; 27x20 cm., ilustraciones y mapas en color. Bibliografía. 900 gr. (A-305-ID-C).
Anbieter: SpringBooks, Berlin, Deutschland
Hardcover. Zustand: Very Good. Reprint with Extras Online instead of CD (link is working). A minimum of wear. Immediately dispatched from Germany.
Sprache: Englisch
Verlag: Berlin / Heidelberg, Springer-Verlag, 2006
ISBN 10: 3540243291 ISBN 13: 9783540243298
Anbieter: Antiquariat Andree Schulte, Grafschaft-Ringen, Deutschland
Verbandsmitglied: GIAQ
XXII, 568 pp + 1 DVD. -TEXT IN ENGLISH- Sprache: Englisch Gewicht in Gramm: 1700 4to. Hardcover, no dust jacket, fine.
Taschenbuch. Zustand: Neu. The Andes | Active Subduction Orogeny | Onno Oncken (u. a.) | Taschenbuch | Frontiers in Earth Sciences | xxii | Englisch | 2017 | Springer | EAN 9783662517833 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.
Sprache: Englisch
Verlag: Springer Berlin Heidelberg, 2017
ISBN 10: 3662517833 ISBN 13: 9783662517833
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Convergent plate margins and subduction zones are first order features shaping the Earth. Convergent continental margins combine the majority of processes that affect the internal architecture thermal and geochemical character of continental lith- phere. In addition, the close relationships between active deformation and uplift, m- matism and associated crustal growth, ore formation, the release of more than 90% of global seismic energy at convergent margins, make these plate boundaries imp- tant natural laboratories where mass and energy flux rates can be studied at various scales. Since the advent of plate tectonic theory, it has been recognized that all of these phenomena are intimately related and often governed by feedback mechanisms. Accordingly, subduction orogeny has become an international, high-priority theme in process-oriented, earth-system analysis. In this context, Dewey and Bird (1970) have defined the Andes as the type representative for orogeny and associated p- cessesat convergent margins in their benchmark paper. The Andes, therefore, p- vide an excellent natural laboratory for studying the above processes.