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100%: Ruff, Larry J. and Kanamori, H.: [Subduction Zones: Part 2] (By: [published: December, 1988] (ISBN: 9783764322724) 2013, Erstausgabe, in Englisch, Taschenbuch.Nur diese Ausgabe anzeigen…
46%: Larry J. Ruff, Larry J. Ruff (Editor), Hiroo Kanamori (Editor): Subduction Zones, Part 1 (ISBN: 9780817619282) Birkhauser Verlag, in Englisch, Broschiert.Nur diese Ausgabe anzeigen…
37%: Ruff, Larry J, and Kanamori, Hiroo (Editor): Subduction Zones, Part II (ISBN: 9780817622725) 1989, in Englisch, Broschiert.Nur diese Ausgabe anzeigen…
[Subduction Zones: Part 2] (By: [published: December, 1988]
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|---|---|---|---|---|
| Schnitt | € 29,49 | € 76,01 | € 85,72 | € 53,49 |
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SUBDUCTION ZONES PART II (PAGEOPH TOPICAL VOLUMES)
DE PBISBN: 9783764322724 bzw. 3764322721, in Deutsch, Birkenhäuser Verlag, Basel/Boston/Stuttgart, Schweiz, Taschenbuch.
Lieferung aus: Indien, plus shipping.
Von Händler/Antiquariat, Books WorldWide Express.
Softcover. Brand New. “International Editionö - ISBN number and front cover may be different in rare cases but contents are same as the US edition. FOR MULTIPLE ORDERS AND EXPEDITE ORDERS, WE USE FEDEX/UPS/DHL SERVICE & RECEIVE FAST WITHIN 3-5 BUSINESS DAYS. No shipping to PO BOX, APO, FPO addresses. Kindly provide day time phone number in order to ensure smooth delivery. Printed in black & white in English language. Territorial restrictions may be printed on the book. We may ship from Asian regions for inventory purpose. 100% Customer satisfaction guaranteed! We use Fast Shipping via DHL/FEDEX/UPS.
Von Händler/Antiquariat, Books WorldWide Express.
Softcover. Brand New. “International Editionö - ISBN number and front cover may be different in rare cases but contents are same as the US edition. FOR MULTIPLE ORDERS AND EXPEDITE ORDERS, WE USE FEDEX/UPS/DHL SERVICE & RECEIVE FAST WITHIN 3-5 BUSINESS DAYS. No shipping to PO BOX, APO, FPO addresses. Kindly provide day time phone number in order to ensure smooth delivery. Printed in black & white in English language. Territorial restrictions may be printed on the book. We may ship from Asian regions for inventory purpose. 100% Customer satisfaction guaranteed! We use Fast Shipping via DHL/FEDEX/UPS.
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Subduction Zones Part Ii (Pageoph Topical Volumes)
DE NWISBN: 9783764322724 bzw. 3764322721, in Deutsch, Db Springer, neu.
Lieferung aus: Indien, plus shipping.
Von Händler/Antiquariat, Textbooks Dealing.
Db Springer. Brand New. ORIGINAL EDITION. Get it fast within 3-5 business days by FEDEX/UPS/DHL with Tracking Number. Kindly provide day time phone number in order to ensure smooth delivery. No shipping to PO BOX, APO, FPO addresses.We may ship from Asian regions for inventory purpose.100% Customer satisfaction guaranteed!
Von Händler/Antiquariat, Textbooks Dealing.
Db Springer. Brand New. ORIGINAL EDITION. Get it fast within 3-5 business days by FEDEX/UPS/DHL with Tracking Number. Kindly provide day time phone number in order to ensure smooth delivery. No shipping to PO BOX, APO, FPO addresses.We may ship from Asian regions for inventory purpose.100% Customer satisfaction guaranteed!
3
Subduction Zones Part II
~EN PB NWISBN: 9783764322724 bzw. 3764322721, vermutlich in Englisch, Springer Nature, Taschenbuch, neu.
Lieferung aus: Deutschland, Lagernd, zzgl. Versandkosten.
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 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. Soft cover.
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 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. Soft cover.
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Subduction Zones Part II (Pageoph Topical Volumes) (2013)
EN PB NW FEISBN: 9783764322724 bzw. 3764322721, in Englisch, 282 Seiten, Birkhäuser, Taschenbuch, neu, Erstausgabe.
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Von Händler/Antiquariat, Wiltonbooks.
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 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. Paperback, Edition: 1, Label: Birkhäuser, Birkhäuser, Product group: Book, Published: 2013-10-04, Release date: 2013-10-04, Studio: Birkhäuser.
Von Händler/Antiquariat, Wiltonbooks.
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 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. Paperback, Edition: 1, Label: Birkhäuser, Birkhäuser, Product group: Book, Published: 2013-10-04, Release date: 2013-10-04, Studio: Birkhäuser.
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Subduction Zones: Part 2
EN NWISBN: 9783764322724 bzw. 3764322721, in Englisch, Birkhauser Verlag AG, neu.
Lieferung aus: Vereinigtes Königreich Großbritannien und Nordirland, in-stock.
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 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.
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 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.
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Subduction Zones
EN PB USISBN: 9780817622725 bzw. 0817622721, in Englisch, Birkhauser, Taschenbuch, gebraucht.
Lieferung aus: Vereinigte Staaten von Amerika, Versandkosten nach: USA.
Von Händler/Antiquariat, Books Express.
Birkhauser. Paperback. Good. We ship International with Tracking Number! May not contain Access Codes or Supplements. Buy with confidence, excellent customer service! j.
Von Händler/Antiquariat, Books Express.
Birkhauser. Paperback. Good. We ship International with Tracking Number! May not contain Access Codes or Supplements. Buy with confidence, excellent customer service! j.
7
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Subduction Zones (1988)
EN PBISBN: 9780817619282 bzw. 0817619283, in Englisch, Birkhauser, Taschenbuch.
Lieferung aus: Vereinigte Staaten von Amerika, Versandkosten nach: USA.
Von Händler/Antiquariat, Ergodebooks.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
Von Händler/Antiquariat, Ergodebooks.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
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