Oceanic lithosphere (34 Ergebnisse)

Hard Cover. Zustand: Fine. No Jacket. Hardcover; includes CD-ROM; in fine condition.

gebundene Ausgabe. Zustand: Gut. 229 Seiten; Der Erhaltungszustand des hier angebotenen Werks ist trotz seiner Bibliotheksnutzung sehr sauber. Es befindet sich neben dem Rückenschild lediglich ein Bibliotheksstempel im Buch; ordnungsgemäß entwidmet. Der Bucheinband ist leicht staubschutzig. In ENGLISCHER Sprache. Sprache: Englisch Gewicht in Gramm: 490.…

Zustand: Poor. Volume 4. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Book contains pencil markings. In poor condition, suitable as a reading copy. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,950grams, ISBN:0792302559.…

Hardcover. Zustand: Gut. 229 p. Good. Ex-library with usual markings. Isolated penciled underlinings. Stamp on edge. Sprache: Englisch Gewicht in Gramm: 560.

Hardcover. Zustand: Fair. No Jacket. Condition : Fair/ very usable study copy. Ex university library with associated markings. Hard cover, no jacket. 413pp. No highlighting or annotations to main text. Faint pencilled ticks on contents page. PAGE CREASING to last few pages. Photo on request.

10pp, 13 figs, Printed Card Cover, VGC.

14pp, 4 figs, Printed Card Cover, VGC.

Zustand: Fair. Volume 7. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Clean from markings. In fair condition, suitable as a study copy. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,2700grams, ISBN:0471028703.…

Hardcover. Zustand: Very Good. No Jacket. Missing dust jacket; May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less.

Zustand: Good. Former library copy. Pages intact with minimal writing/highlighting. The binding may be loose and creased. Dust jackets/supplements are not included. Includes library markings. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.

Hardcover. Zustand: Gut. 229 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. D03437 354008276X Sprache: Englisch Gewicht in Gramm: 550.

Hardcover w dj. Zustand: Very Good. Prompt Shipment, shipped in Boxes, Tracking PROVIDED; VERY Good or Better hardcover, sm4to, 413 pp.

Cloth. Zustand: Gut. 413 pages. Good. Dust jacket shows mild wear. Note of ownership on title page. Otherwise clean pages. Sprache: Deutsch Gewicht in Gramm: 1150.

Hardcover. Zustand: Gut. 903 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w09328 792311760 Sprache: Englisch Gewicht in Gramm: 1100.

Softcover. Zustand: Wie neu. 1. Auflage. Das Buch ist in einem sehr guten Zustand / Unbenutzt.

Zustand: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.…

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Ophiolites are key sources of information regarding the genesis and evolution of oceanic lithosphere. Over the past decades, the geological ~tudy of ophio lites has provided a wealth of insight into lithospheric processes and has proved to be an indispensible prerequisite to interpreting geophysical and other investigations of the crust underlying recent oceans. The Oman Ophiol ite offers the most complete and structurally undisturbed sections of the oceanic crust in vast, clean exposures. It is, therefore, most fortunate for the scientific community that Mhd. Kassim, Director General of Minerals and Dr. Hilal Al Azri, Director of the Geological Survey, took upon themselves the task of organizing in Oman an international meeting on ophiolites. Having planned for an attendance of only 100 to 150 persons, the logistics of the organizing committee were put to a severe test by th~ 300 participants who eventually arrived from 27 countries. The 14 field trips, most of which were conducted twice, provided the participants with an excellent introduc tion to the geology of Oman, the ophIolite sequence, and re~ated phenomena.…

Zustand: New. In.

Zustand: Gut. Formateinband: Ringbuch 285 S. 1. Aufl.; (Mit Abbildungen); Am Hinterdeckel teils fleckig; sonst in gutem Zustand. Sprache: Englisch Gewicht in Gramm: 490 [Stichwörter: Feldexkursionen, Handbuch].

Zustand: New. In.

Zustand: New. This book, first published in 2004, reviews the subject of the nature, causes, and consequences of fluid flow in oceanic crust. Editor(s): Davis, Earl E.; Elderfield, Harry. Num Pages: 728 pages, 20 tables. BIC Classification: RBG; RBKC. Category: (P) Professional & Vocational; (U) Tertiary Education (US: College). Dimension: 244 x 170 x 37. Weight in Grams: 1140. . 2013. Paperback. . . . . Books ship from the US and Ireland. …

Paperback. Zustand: Brand New. 706 pages. 9.50x6.75x1.75 inches. In Stock.

Zustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In good all round condition. Dust jacket in fair condition. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1100grams, ISBN:9780632012190.…

Taschenbuch. Zustand: Neu. Heat and Fluid Flow at a Crustal Scale | Observations and Models of Coupled Transport in Young Oceanic Lithosphere | Michael Hutnak | Taschenbuch | 460 S. | Englisch | 2013 | LAP LAMBERT Academic Publishing | EAN 9783659417603 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Norderstedt, info[at]bod[dot]de | Anbieter: preigu. …

Paperback. Zustand: Brand New. 238 pages. 8.90x5.98x0.55 inches. In Stock.

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - I was invited to write this book as part of the Minerals, Rocks and Organic Materials Series of Springer-Verlag by Professor Peter J. Wyllie in 1974. Ophiolites have preoccupied me ever since 1948 as a graduate student and up to the present time as part of my research with the U.S. Geological Survey. During this period ophiolite, an obscure European geological term, has attained an ever-increasing importance, is now used to include all fragments of ancient oceanic lithosphere incorporated into the orogenic zones of modern and ancient continental margins, and is a standard part of the plate tectonic paradigm. The purpose of this book is to provide a starting point for anyone interested in the background and state of knowledge concerning ophiolites (ancient oceanic lithosphere). Because ophiolites represent fragments of old oceanic crust their tectonic setting and age are extremely important in the reconstruction of ancient plate boundaries. Present day plate tectonic theories involve the generation and disposal of oceanic lithosphere, so that these ancient fragments of oceanic lithosphere can be used directly to reconstruct conditions within the ancient oceans. Since 1970, numerous meetings and conferences directly related to ophiolites have stimulated worldwide interest in the subject. As part of the International Correlation Program, the project 'Ophiolites of Continents and Comparable Oceanic Rocks,' was initiated by Dr. N. Bogdanov, Geological Institute, Moscow. This project has brought together an international group that has focused on the outstanding problems and is now producing a world map of ophiolite distribution.…

Zustand: New. In.

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Originally published in 2004, this is a comprehensive review of the subject of the nature, causes, and consequences of fluid flow in oceanic crust, setting in context much research for the first time. The book begins with a concise review of the relatively brief history of its subject which began shortly after the dawning of plate-tectonic theory. It then describes the nature and important consequences of fluid flow in the sub-seafloor, ending with a summary of how the oceans are affected by the surprisingly rapid exchange of water between the crust and the water column overhead. The accompanying internet material includes a full and easily navigated set of diagrams and captions, references, and photos of research vessels, submersibles, and tools used in marine hydrologic studies. A valuable resource for graduate students and researchers of Earth Sciences and Oceanography.…

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - 1.1. HISTORICAL DEVELOPMENT OF THE OPHIOLITE CONCEPT. Ophiolite, Greek for 'the snake stone', appears to have received its first written definition by Brongniart (1813) as a serpentine matrix containing various minerals. Later in 1821 and 1827, Brongniart determined that volcanic and gabbroic rocks were also present, associated with cherts, and he ascribed an igneous origin to the ophiolite. Amstutz (1980) gives an excellent exegesis of these early contributions and traces the further use of the term and concept of ophiolite. This concept had been forged in the western Alps and Apennines where, thanks to talented Italian geologists, in particular A. Sismonda, B. Gastaldi, V. Novarese and S. Franchi, the study on metamorphic ophiolites (the 'pietre verdi') has rapidly progressed. At the tum of the century the association of radiolarite, diabase, gabbro (euphotide), and serpentinite-peridotite was clearly identified, even through their metamorphic transformations. In 1902, Franchi developed the hypothesis introduced earlier by Lotti (1886), of a submarine outflow to explain the 'pietre verdi' association, on the basis of the attribution of the variolites and metamorphic prasinites to an hypabyssal volcanism, also responsible for the formation of radiolarites. Thus, before the popular work of Steinmann in 1927, the various components constituting an ophiolite had been identified and its hypabyssal origin proposed. As recalled by Amstutz (1980), the so-called 'Steinmann trinity', which consists of the association of radiolarites, diabases and serpentinites, was more completely and better defined in these earlier works. …

Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - 1.1. HISTORICAL DEVELOPMENT OF THE OPHIOLITE CONCEPT. Ophiolite, Greek for 'the snake stone', appears to have received its first written definition by Brongniart (1813) as a serpentine matrix containing various minerals. Later in 1821 and 1827, Brongniart determined that volcanic and gabbroic rocks were also present, associated with cherts, and he ascribed an igneous origin to the ophiolite. Amstutz (1980) gives an excellent exegesis of these early contributions and traces the further use of the term and concept of ophiolite. This concept had been forged in the western Alps and Apennines where, thanks to talented Italian geologists, in particular A. Sismonda, B. Gastaldi, V. Novarese and S. Franchi, the study on metamorphic ophiolites (the 'pietre verdi') has rapidly progressed. At the tum of the century the association of radiolarite, diabase, gabbro (euphotide), and serpentinite-peridotite was clearly identified, even through their metamorphic transformations. In 1902, Franchi developed the hypothesis introduced earlier by Lotti (1886), of a submarine outflow to explain the 'pietre verdi' association, on the basis of the attribution of the variolites and metamorphic prasinites to an hypabyssal volcanism, also responsible for the formation of radiolarites. Thus, before the popular work of Steinmann in 1927, the various components constituting an ophiolite had been identified and its hypabyssal origin proposed. As recalled by Amstutz (1980), the so-called 'Steinmann trinity', which consists of the association of radiolarites, diabases and serpentinites, was more completely and better defined in these earlier works.…