Larry ruff (11 risultati)
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Da: Research Ink, Takoma Park, MD, U.S.A.Research Ink
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EUR 20,75
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Paperback. Condizione: Very Good. 282 pp. Pageoph Topical Volumes. Rubber-stamped on front free endpaper. book.
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Da: Kennys Bookshop and Art Galleries Ltd., Galway, GY, IrlandaKennys Bookshop and Art Galleries Ltd.
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EUR 49,73
EUR 10,50 spedizioneSpedito da Irlanda a U.S.A.Quantità: 15 disponibili
Condizione: New. Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 1/2 Series: Pageoph Topical Volumes. Num Pages: 287 pages, biography. BIC Classification: YQS. Category: (P) Professional & Scholarly; (UP) Postgraduate; (UU) Undergraduate. Dimension: 244 x 170 x 15. Weight in Grams: 605. . 1988. Paperba…ck. . . . .
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Da: Ria Christie Collections, Uxbridge, Regno UnitoRia Christie Collections
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EUR 53,84
EUR 13,90 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Condizione: New. In.
- Brossura
Da: Revaluation Books, Exeter, Regno UnitoRevaluation Books
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EUR 55,51
EUR 14,51 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 2 disponibili
Paperback. Condizione: Brand New. 1st edition. 292 pages. German language. 9.61x6.69x0.66 inches. In Stock.
- Brossura
Da: Kennys Bookstore, Olney, MD, U.S.A.Kennys Bookstore
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EUR 62,17
EUR 9,19 spedizioneSpedito in U.S.A.Quantità: 15 disponibili
Condizione: New. Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 1/2 Series: Pageoph Topical Volumes. Num Pages: 287 pages, biography. BIC Classification: YQS. Category: (P) Professional & Scholarly; (UP) Postgraduate; (UU) Undergraduate. Dimension: 244 x 170 x 15. Weight in Grams: 605. . 1988. Paperba…ck. . . . . Books ship from the US and Ireland.
Altre immagini- Brossura
Da: Antiquariat Bookfarm, Löbnitz, GermaniaAntiquariat Bookfarm
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EUR 60,00
EUR 40,00 spedizioneSpedito da Germania a U.S.A.Quantità: 1 disponibili
gr.-8°, broschiert. S. 449-800; 282 S. Zwei Bände. Mehrbändiges ehemaliges Bibliotheksexemplar mit Stempeln und Rückensignaturen. Einbände mit leichten Lagerspuren, Papier etwas nachgedunkelt, vereinzelte kleine Anstreichungen möglich. Dem Alter entsprechend guter Zustand. mbx 3764322721 Sprache: Englisch Gewicht in Gramm: 1450…Reprint from Pure and applied geophysics (PAGEOPH), Vol. 28, 1988, no. 3/4. T. p. verso.
- Brossura
Da: AHA-BUCH GmbH, Einbeck, GermaniaAHA-BUCH GmbH
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 53,49
EUR 62,54 spedizioneSpedito da Germania a U.S.A.Quantità: 2 disponibili
Taschenbuch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic lithosphere production system which can be linked as a nearly continuous, albeit sinuous, strand around the earth, subduction zones a…re a rather dissociated group and are found in several isolated corners of the world. While plate tectonics can predict that subduction zones are required along certain plate boundaries, it does not stipulate how subduction zones initiate and develop. The preservation of newly created oceanic lithosphere and the propensity for spreading centers to fragment continents leaves a wealth of geological informa tion on the initiation and evolution of spreading. On the other hand, the subject of subduction initiation has little observational basis. To find such observations, we need to look at some muddled tectonic regimes. The Macquarie Ridge complex presents a natural laboratory for studies of subduction initiation. 2. Tectonics of the Macquarie Ridge Complex The Macquarie Ridge complex is a complicated physiographic feature that trends approximately north-south between South Island, New Zealand and the Pacific-Antarctica spreading center. This feature consists of a sequence of troughs and ridges, with Macquarie Island as the only exposed expression. The seismically active Macquarie Ridge complex (hereafter: MRC) is crudely continuous with the Tonga-Kermadec-New Zealand seismic activity. The basic physiographic features and seismicity of the MRC are shown in Figure I. The earthquake epicenters generally cluster about the bathymetric expression of the MRC.
- Brossura
Da: Mispah books, Redhill, SURRE, Regno UnitoMispah books
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EUR 107,59
EUR 29,02 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Paperback. Condizione: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.
- Brossura
- Print on Demand
Da: moluna, Greven, Germaniamoluna
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EUR 44,39
EUR 48,99 spedizioneSpedito da Germania a U.S.A.Quantità: Più di 20 disponibili
Kartoniert / Broschiert. Condizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 1/2Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic… lithosphere production system which can be linked as a nearly.
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- Print on Demand
Da: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, GermaniaBuchWeltWeit Ludwig Meier e.K.
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EUR 85,55
EUR 23,00 spedizioneSpedito da Germania a U.S.A.Quantità: 2 disponibili
Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic lithosphere production system which can be linked as a nearly continuous, albeit sinuous, strand around the earth, su…bduction zones are a rather dissociated group and are found in several isolated corners of the world. While plate tectonics can predict that subduction zones are required along certain plate boundaries, it does not stipulate how subduction zones initiate and develop. The preservation of newly created oceanic lithosphere and the propensity for spreading centers to fragment continents leaves a wealth of geological informa tion on the initiation and evolution of spreading. On the other hand, the subject of subduction initiation has little observational basis. To find such observations, we need to look at some muddled tectonic regimes. The Macquarie Ridge complex presents a natural laboratory for studies of subduction initiation. 2. Tectonics of the Macquarie Ridge Complex The Macquarie Ridge complex is a complicated physiographic feature that trends approximately north-south between South Island, New Zealand and the Pacific-Antarctica spreading center. This feature consists of a sequence of troughs and ridges, with Macquarie Island as the only exposed expression. The seismically active Macquarie Ridge complex (hereafter: MRC) is crudely continuous with the Tonga-Kermadec-New Zealand seismic activity. The basic physiographic features and seismicity of the MRC are shown in Figure I. The earthquake epicenters generally cluster about the bathymetric expression of the MRC. 282 pp. Englisch.
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- Print on Demand
Da: buchversandmimpf2000, Emtmannsberg, BAYE, Germaniabuchversandmimpf2000
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EUR 53,49
EUR 60,00 spedizioneSpedito da Germania a U.S.A.Quantità: 1 disponibili
Taschenbuch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic lithosphere production system which can be linked as a nearly continuous, albeit sinuous, strand around the earth, subduc…tion zones are a rather dissociated group and are found in several isolated corners of the world. While plate tectonics can predict that subduction zones are required along certain plate boundaries, it does not stipulate how subduction zones initiate and develop. The preservation of newly created oceanic lithosphere and the propensity for spreading centers to fragment continents leaves a wealth of geological informa tion on the initiation and evolution of spreading. On the other hand, the subject of subduction initiation has little observational basis. To find such observations, we need to look at some muddled tectonic regimes. The Macquarie Ridge complex presents a natural laboratory for studies of subduction initiation. 2. Tectonics of the Macquarie Ridge Complex The Macquarie Ridge complex is a complicated physiographic feature that trends approximately north-south between South Island, New Zealand and the Pacific-Antarctica spreading center. This feature consists of a sequence of troughs and ridges, with Macquarie Island as the only exposed expression. The seismically active Macquarie Ridge complex (hereafter: MRC) is crudely continuous with the Tonga-Kermadec-New Zealand seismic activity. The basic physiographic features and seismicity of the MRC are shown in Figure I. The earthquake epicenters generally cluster about the bathymetric expression of the MRC.Springer Nature c/o IBS, Benzstrasse 21, 48619 Heek 292 pp. Englisch.
