Roberts proctor (24 Ergebnisse)
Verlag: UMR Journal, April 1968, 156 Pp., 1968
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Sprache: Englisch
Verlag: Dordrecht: Kluwer, 1992
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Großformat, Original-Pappband. 427 Seiten mit zahlreichen s/w Abbildungen. Gutes Exemplar mit nur leichten Gebrauchsspuren. Textsauber und aus einem Nichtraucherhaushalt. Dieses Exemplar stammt aus der Bibliothek von Dr. Volker Hellmann, ehemaliger Dozent am Fachbereich Biologie der Universität Konstanz. // Original hardcover. A… good copy with only minor signs of use. The text is clean, and it comes from a non-smoking household. This copy comes from the library of Dr. Volker Hellmann, former lecturer at the Department of Biology at the University of Konstanz. Book with many b/w illustrations. Sprache: Englisch.

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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.

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Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - B. A. ROBERTS&J. PROCTOR The term 'serpentine' referring to rocks and min of each of the polymorphs. These conditions in erals, can be traced back to the ancient Roman clude temperatures of generally less than 530°C, era of Dioscorides (A. D. 50) (Fa…ust & Fahey and fluid pH's in excess of 10 with low pC02 Serpentine protoliths are essentially ultramafic 1962) and they suggest that the speckled colour of serpents and the fact that Dioscorides recom rocks which fall into a number of categories: (a) mended it for the prevention of snakebite as two stratiform complexes, (b) concentrically zoned complexes, (c) ophiolite complexes and, (d) high of many origins of the name. It is well known that the use of serpentinized rocks by sculptors temperature peridotite complexes. The most and carvers since ancient times is a tradition that commonly recognized are generally assigned to the ophiolite suite (Malpas, Ch. 2, this is still carried on today (Fig. 1). The differences in chemical composition of serpentinized rocks volume) and occur in most fold-mountain belts are many and specimens come in a wide range of of the world. Serpentinized ultramafic rocks attractive solid and mixed colours, e. g. , red, 'H4(MgFe hSi20 9, approximate composition) green, blue and black.

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Zustand: gut. 1992. The Ecology of Areas with Serpentinized Rocks: A World View. Geobotany 17. In englischer Sprache. pages.

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LeatherBound. Zustand: New. BOOKS ARE EXEMPT FROM IMPORT DUTIES AND TARIFFS; NO EXTRA CHARGES APPLY. LeatherBound edition. Condition: New. Reprinted from 1854 edition. Leather Binding on Spine and Corners with Golden leaf printing on spine. Bound in genuine leather with Satin ribbon page markers and Spine with raised gilt bands.… A perfect gift for your loved ones. Pages: 52 NO changes have been made to the original text. This is NOT a retyped or an ocr'd reprint. Illustrations, Index, if any, are included in black and white. Each page is checked manually before printing. As this print on demand book is reprinted from a very old book, there could be some missing or flawed pages, but we always try to make the book as complete as possible. Fold-outs, if any, are not part of the book. If the original book was published in multiple volumes then this reprint is of only one volume, not the whole set. Sewing binding for longer life, where the book block is actually sewn (smythe sewn/section sewn) with thread before binding which results in a more durable type of binding. Pages: 52 St. John's Hospital (Stone, Buckinghamshire, England),Carrington, G, Jr,Brandon, D,Millar, John,Fryer, Jane,Hollyer, Richard Roberts,Mylne, J. W,Hume, J. R,Proctor, B. W,Gaskell, S.
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Dordrecht, Kluwer Academic, 1992. 427 pp. Col. & b./w. ills. Orig. hardcover. (Geobotany, 17).
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Taschenbuch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -B. A. ROBERTS&J. PROCTOR The term 'serpentine' referring to rocks and min of each of the polymorphs. These conditions in erals, can be traced back to the ancient Roman clude temperatures of generally less than 530°C, era of Dioscoride…s (A. D. 50) (Faust & Fahey and fluid pH's in excess of 10 with low pC02 Serpentine protoliths are essentially ultramafic 1962) and they suggest that the speckled colour of serpents and the fact that Dioscorides recom rocks which fall into a number of categories: (a) mended it for the prevention of snakebite as two stratiform complexes, (b) concentrically zoned complexes, (c) ophiolite complexes and, (d) high of many origins of the name. It is well known that the use of serpentinized rocks by sculptors temperature peridotite complexes. The most and carvers since ancient times is a tradition that commonly recognized are generally assigned to the ophiolite suite (Malpas, Ch. 2, this is still carried on today (Fig. 1). The differences in chemical composition of serpentinized rocks volume) and occur in most fold-mountain belts are many and specimens come in a wide range of of the world. Serpentinized ultramafic rocks attractive solid and mixed colours, e. g. , red, 'H4(MgFe hSi20 9, approximate composition) green, blue and black. 444 pp. Englisch.

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Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Section I Introduction.- I. Introduction.- Section II Geology.- II. Serpentine and the geology of serpentinized rocks.- Section III North America.- III. Plant life of western North American ultramafics.- IV. Ecology of…serpentinized areas, Newfoundland, Can.

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Taschenbuch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -B. A. ROBERTS&J. PROCTOR The term 'serpentine' referring to rocks and min of each of the polymorphs. These conditions in erals, can be traced back to the ancient Roman clude temperatures of generally less than 530°C, era of Dioscorides (A…. D. 50) (Faust & Fahey and fluid pH's in excess of 10 with low pC02¿ Serpentine protoliths are essentially ultramafic 1962) and they suggest that the speckled colour of serpents and the fact that Dioscorides recom rocks which fall into a number of categories: (a) mended it for the prevention of snakebite as two stratiform complexes, (b) concentrically zoned complexes, (c) ophiolite complexes and, (d) high of many origins of the name. It is well known that the use of serpentinized rocks by sculptors temperature peridotite complexes. The most and carvers since ancient times is a tradition that commonly recognized are generally assigned to the ophiolite suite (Malpas, Ch. 2, this is still carried on today (Fig. 1). The differences in chemical composition of serpentinized rocks volume) and occur in most fold-mountain belts are many and specimens come in a wide range of of the world. Serpentinized ultramafic rocks attractive solid and mixed colours, e. g. , red, «H4(MgFe hSi20 9, approximate composition) green, blue and black.Springer-Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 444 pp. Englisch.

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