gerhard voll (20 resultados)

Broschur. Condición: gut. 25 cm, Abb., handschr. Widmung von Nabholz, Einband leicht fleckig, leicht geknickt, Besitzvermerk, aus der Sammlung Alexander Tollmann. Sprache: deu.

Condición: gut. 382 S. : Ill., graph. Darst., Kt. + 5 Beil. in Tasche, 25 cm, Bibliotheksexemplar, Einband geknickt und leicht beschädigt, gebräunt, Vorblatt stockfleckig, Inhalt gut erhalten. Sprache: Deutsch.

8°, Broschur, 382 Seiten, 5 Tafeln, 96 Abbildungen, 17 Tabellen, geringe Gebrauchsspuren an Einband und Block, Block sauber und fest Deutsch 300g.

paperback. Condición: Gut. Seiten; Thieme - 2. Auf. 2000 : Gerhard K. Lang - tb - 9-48-4-L2 W3-XECI-ZL7K Sprache: Deutsch Gewicht in Gramm: 1.

Hardcover. XIII, 484 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. w10263 3540532730 Sprache: Englisch Gewicht in Gramm: 550.

Hardcover. XIII, 484 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. w09690 3540532730 Sprache: Englisch Gewicht in Gramm: 1100.

Gr. 8°, OKart. 1. Aufl. Mit 5 Tafeln (gut erhaltene, beiliegende und ausfaltbare Karten), 96 Abbild., 17 Tabellen, 382 S. Widmung des Autoren auf Vorderdeckel, Einband minimal berieben, sonst schönes Ex. Sprache: Deutsch Gewicht in Gramm: 0.

Condición: New. In.

Condición: New.

Condición: New. pp. 512.

Paperback. Condición: Brand New. 512 pages. 9.60x6.70x1.20 inches. In Stock.

Taschenbuch. Condición: Neu. Druck auf Anfrage Neuware - Printed after ordering - With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism.

4°, Pp., gebundene Ausgabe. 60 S. : zahlr. Ill. ; 32 cm, 692 gr. Einband mit leichten Lagerspuren, sonst sehr gut erhalten. Sprache: Deutsch Gewicht in Gramm: 794.

Softcover. Condición: Gut. 1. Auflage. Beihefte zum Geologischen Jahrbuch 42. 382 S. Mit 5 Tafeln, 96 Abbildungen und 17 Tabellen.Großoktav. Or. br. Vermerk auf dem Umschlag. Rücken fleckig. Sonst gut. Innen sehr sauber mit Papierbräunung. Buch.

brosch. Condición: Gut. 382 S., 3 Ktn. Beil. in Rückentasche : Mit 5 Taf., 96 Abb. u. 17 Tab. ; gr. 8 Gestempelt, sonst guter Zustand. AG1068 Sprache: Deutsch Gewicht in Gramm: 1001.

Condición: new. Questo è un articolo print on demand.

Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism. 512 pp. Englisch.

Condición: New. Print on Demand pp. 512.

Condición: New. PRINT ON DEMAND pp. 512.

Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 512 pp. Englisch.