W d j koch (68 resultados)

Paperback. Condición: New.

Paperback. Condición: New.

ISBN 3-8237-5550-1 448 S 23,5x16,5cm, illustr. Hardcover, Fotos und Abbildungen im Text, gutes Exemplar.

Hardcover. Gr.-8° ( 23 : 16 cm). Neuerer Halbleinenband mit goldgeprägtem Rückentitel. (4), 570 Seiten mit sehr zahlreichen Abbildungen, Skizzen, Diagrammen etc. Auf dem vorderen Vorsatz mit Stempel: Mit den besten Empfehlungen überreicht von P. A. Thiessen. Mit eingebunden zwei Gedenkphotos für Uffz. Konrad Bläsius, gef. als Fallschirmjäger auf Kreta 20.5.1941 und Uffz. Heinz Böge, gef. 22.7.1941 in Rußland. Innen wie außen sauber, gutes Exemplar. Es handelt sich um gesammelte Sonderabdrucke aus diversen Fachzeitschriften wie z.B.: VDI-Beihefte, Ztschr. für anorg. und allgem. Chemie, Ztschr. für physik. Chemie, Justus Liebig's Annalen der Chemie, aber auch um Vorträge bei versch. Institutionen. Beiträge unter anderem von . -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Genießen Sie den goldenen Herbst! Machen Sie es sich gemütlich , bei uns finden Sie sicher die passende Lektüre! -- Wir kaufen Ihre werthaltigen Bücher! Chem.…

Condición: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV2. softcover, wrapped in shrink wrap, tight, crisp.…

Condición: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV1. softcover, wrapped in shrink wrap, tight, crisp.…

Condición: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea." DV4. softcover, wrapped in shrink wrap, tight, crisp, 4.…

Condición: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. DX1. softcover, wrapped in shrink wrap, tight, crisp, 429.…

Condición: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. softcover, wrapped in shrink wrap, tight, crisp, 429 page.…

Paperback. Condición: New.

Softcover. Condición: Fine. Single Issue. 36pp. Stapled wrappers. Fine. "The American Press vs. de Gaulle" by C. Richard Cleary. Contributions by C. Richard Cleary, Sister Mary Ellen, Charles Edward Eaton, Margaret Alexander, J.M. Dunning, Claude F. Koch, D.L. Winchester, Lawrence P. Spingarn, Daniel Hoffman, Ruth Berman, Laura Burks Alnutt, William Virgil Davis, Donal Mahoney, W.V. Mittnacht, and Matthew Wilson. …

Paperback. Condición: New.

Condición: As New. Unread book in perfect condition.

Condición: New.

Hardcover. Condición: Very Good. 2020 Springer hardcover edition. Light reading wear else very good condition. Contents: 1 Reflexive and Reflective Auditory Feedback, Jens Blauert, Guy J. Brown; 2 Auditory Gestalt Rules and Their Application, Sarinah Sutojo, Joachim Thiemann, Armin Kohlrausch, Steven van de Par; 3 Selective Binaural Attention and Attention Switching, Janina Fels, Josefa Oberem, Iring Koch; 4 Blackboard Systems for Cognitive Audition, Christopher Schymura, Dorothea Kolossa; 5 Formation of Three-Dimensional Auditory Space, Piotr Majdak, Robert Baumgartner, Claudia Jenny; 6 Biological Aspects of Perceptual Space Formation, Michael Pecka, Christian Leibold, Benedikt Grothe; 7 Auditory Spatial Impression in Concert Halls, Tapio Lokki, Jukka Patynen; 8 Auditory Room Learning and Adaptation to Sound Reflections, Bernhard U. Seeber, Samuel Clapp; 9 Room Effect on Musicians' Performance, Malte Kob, Sebastia V. Amengual Gari, Zora Scharer Kalkandjiev; 10 Binaural Modeling from an Evolving-Habitat Perspective, Jonas Braasch; 11 Psychophysical Models of Sound Localisation with Audiovisual Interactions, Catarina Mendonca; 12 Cross-Modal and Cognitive Processes in Sound Localization, M. Torben Pastore, Yi Zhou, William A. Yost; 13 Spatial Soundscape Superposition and Multimodal Interaction, Michael Cohen, William L. Martens; 14 Binaural Evaluation of Sound Quality and Quality of Experience, Alexander Raake, Hagen Wierstorf; 15 The Language of Rooms: From Perception to Cognition to Aesthetic Judgment, Stefan Weinzierl, Steffen Lepa, Martin Thiering; 16 Modeling the Aesthetics of Audio-Scene Reproduction, John Mourjopoulos; 17 A Virtual Testbed for Binaural Agents, Jens Blauert; 18 Binaural Technology for Machine Speech Recognition and Understanding, Richard M. Stern, Anjali Menon; 19 Modeling Binaural Speech Understanding in Complex Situations, Mathieu Lavandier, Virginia Best; 20 Creating Auditory Illusions with Spatial-Audio Technologies, Rozenn Nicol; 21 Creating Auditory Illusions with Binaural Technology, Karlheinz Brandenburg, Florian Klein, Annika Neidhardt, Ulrike Sloma, Stephan Werner; 22 Toward Cognitive Usage of Binaural Displays, Yoiti Suzuki, Akio Honda, Yukio Iwaya, Makoto Ohuchi, Shuichi Sakamoto; 23 Audition as a Trigger of Head Movements, Benjamin Cohen-Lhyver, Sylvain Argentieri, Bruno Gas; 24 Intelligent Hearing Instruments-Trends and Challenges, Eleftheria Georganti, Gilles Courtois, Peter Derleth, Stefan Launer; 25 Scene-Aware Dynamic-Range Compression in Hearing Aids, Tobias May, Borys Kowalewski, Torsten Dau. …

Condición: As New. Unread book in perfect condition.

, hcalf (spine broken, covers taped & heavily worn, library stamp in front) 0.0.

Condición: New.

Broché. Condición: Etat moyen. in-8 Description :Pages 2071-2230. Exemplaire non coupé. Tranche roussie aux coiffes frottées. Couverture défraîchie brunie aux bords frottés. Annotations sur 1er plat. Tranche piquée. Langue : Allemand Nb de volumes : 1.

Broché. Condición: Etat moyen. in-8 Description :Pages 1911-2070. Exemplaire non coupé. Tranche roussie aux coiffes frottées. Couverture défraîchie brunie aux bords frottés. Annotations sur 1er plat. Tranche piquée. Langue : Allemand Nb de volumes : 1.

Broché. Condición: Etat moyen. in-8 Description :Pages 1751-1910. Exemplaire non coupé. Tranche roussie aux coiffes frottées. Couverture défraîchie brunie aux bords frottés. Annotations sur 1er plat. Tranche piquée. Langue : Allemand Nb de volumes : 1.

Broché. Condición: Etat moyen. in-8 Description :Pages 2231-2390. Exemplaire non coupé. Tranche roussie aux coiffes frottées. Couverture défraîchie brunie aux bords frottés. Annotations sur 1er plat. Tranche piquée. Langue : Allemand Nb de volumes : 1.

Broché. Condición: Etat moyen. in-8 Description :Pages 2391-2550. Exemplaire non coupé. Tranche roussie aux coiffes frottées. Couverture défraîchie brunie aux bords frottés. Annotations sur 1er plat. Tranche piquée. Langue : Allemand Nb de volumes : 1.

Broché. Condición: Etat moyen. in-8 Description :Pages 2551-2710. Exemplaire non coupé. Tranche roussie aux coiffes frottées. Couverture défraîchie brunie aux bords frottés. Annotations sur 1er plat. Tranche piquée. Langue : Allemand Nb de volumes : 1.

Hardcover. 8°, Halbleinenband der Zeit mit goldgeprägtem Rückentitel, etwas angestaubt und berieben. IX, 394 (2) Seiten mit eingen Übersichten im Text, zwei davon in Farbe. Vorsatz und Titelblatt mit alten Stempeln und Signaturen, ansonsten gutes, sauberes Exemplar. -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Genießen Sie den goldenen Herbst! Machen Sie es sich gemütlich , bei uns finden Sie sicher die passende Lektüre! -- Wir kaufen Ihre werthaltigen Bücher! K01598J.…

Condición: Good. lx, 844; (ii), 102, . . HB. 8vo, rebound in later cloth (chipped to head of spine). Ex-lib.: book-plate to endpaper; small label removed from spine; ink annotations to fly-leaf. Some occasional spotting/minor marginal staining to text. Some marginal pencil annotations. First edition. Includes Index published 1838. A major early flora that systematically documented the plants of Germany and Switzerland with scientific rigor.Stafleu 3803Daniel Joseph Koch (1771-1849) was a German physician and botanist. In 1824 he was appointed professor of medicine and botany at the University of Erlangen, and later was also director of the botanical gardens. His major publications were the 'Catalogus plantarum, quae in ditione Florae Palatinatus' 1814 as well as the present work.…

Hardcover. Condición: Used - Very Good.

HRD. Condición: New. New Book. Shipped from UK. Established seller since 2000.

HRD. Condición: New. New Book. Shipped from UK. Established seller since 2000.

Small 8vo. Pp. lxxxii,604, index. Contemp. plain cloth. - First edition. Inscribed on front end-paper: " ex libris Ch. Marcel stud. med., Bern 1846" .