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Verlag: Springer-Verlag, 1973
ISBN 10: 3540061568ISBN 13: 9783540061564
Anbieter: Versandantiquariat Christoph Groß, Saarbrücken, Deutschland
Buch
Hardcover. Zustand: Sehr gut. Institutsstempel, with 250 figures, 7 plates and 3 maps, praktisch keine Nutzspuren, sehr gute Erhaltung.
Verlag: Springer-Verlag Berlin and Heidelberg GmbH & Co. K, 1973
ISBN 10: 3540061568ISBN 13: 9783540061564
Anbieter: Ammareal, Morangis, Frankreich
Buch
No jacket. Zustand: Très bon. Légères traces d'usure sur la couverture. Tampon ou marque sur la face intérieure de la couverture. Sans jaquette. Edition 1973. Ammareal reverse jusqu'à 15% du prix net de cet article à des organisations caritatives. ENGLISH DESCRIPTION Book Condition: Used, Very good. Slight signs of wear on the cover. Stamp or mark on the inside cover page. No dust jacket. Edition 1973. Ammareal gives back up to 15% of this item's net price to charity organizations.
Verlag: Berlin Heidelberg New York Springer 1 Auflage VI 471 Seiten Literaturverzeichnis SEITEN 463-471 26 x 175 cm gebunden fadengeheftet, 1973
ISBN 10: 0097835412ISBN 13: 9780097835419
Anbieter: Antiquariat Bernhard, Berlin, Deutschland
Buch
mit 257 Illustrationen, graphischen Darstellungen unddrei Karten in eingeklebter Kartentasche, gut erhaltenes Exemplar, einige geringere Gebrauchsspuren, einige Anstreichungen, Namenseintragung, insgesamt ansehnliches Stück 1050 gr. 1050.
Verlag: Springer Berlin Heidelberg, 2013
ISBN 10: 3642655475ISBN 13: 9783642655470
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Buch
Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - This volume, although not an integrated synthesis, treats most aspects of Holocene sedimenta tion and diagenesis in the Persian Gulf, grouping 22 contributions under a single cover and in one language. Because these sediments and diagenetic minerals are comparable to those existing in many ancient sedimentary basins, their appraisal should be of value to the enlarging group of workers who interpret ancient sedimentary rocks. The essential morphological, climatic and oceanographic factors determining Holocene sedimen tation and diagenesis in the Persian Gulf are summarized in the introductory article by PURSER and SEIBOLD. These environmental controls and the overall morphology of the Persian Gulf have much in common with Shark Bay, Western Australia, described by LOGAN et al. (1970). On the other hand, the Persian Gulf is markedly different from the better known Florida and Bahamian prov inces; the floor of the Persian Gulf is gently inclined from continental shoreline to bathymetric axis (80-100 m); the Bahamian province, on the other hand, is horizontal and extremely shallow (2-10 m), with very sharply defined shelf edges surrounded by deep oceanic waters. These contrast ing architectural styles are related to different tectonic frames.