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Evolution in Mixed Populations of Tribolium (pp. 357-365) AND Competiton Between Metal Tolerant and Normal Plant Populations on Normal Soil (pp. 366-372). (FROM: Evolution, Vol. 26, No. 3, September 1972).
Dawson, Peter S.; Sheila C. A. Cook, Claude Lefebvre and Thomas McNeilly.
Editore: Evolution., 1972
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Aggiungi al carrelloNo Binding. Condizione: Very Good. ORIGINAL Articles, disbound from journal; no covers; in very good condition. Journal.
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perfect. Condizione: Gut. 464 Seiten; B2415-19 3426671018 Sprache: Deutsch Gewicht in Gramm: 500.
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perfect. Condizione: Gut. 464 Seiten; B1897-31 3426671018 Sprache: Deutsch Gewicht in Gramm: 500.
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The Yearbook of Landscape Architecture: The Issues of Energy
Richard L. Austin, Kerry Dawson, Thomas A. Musiak, William Scerbo
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Hardcover. Condizione: Fine. Condizione sovraccoperta: Very Good. Hardcover, with dust jacket. 116 pgs. Fine in VG dj, with moderate wear to top edge.
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Advanced Paediatric Life Support: The Practical Approach
Advanced Life Support Group; Tylee; Dawson; Hatcher; Group, Advanced Life Support; Malik; McCluskey; Stewart; Fay; Krieger, Sharon; Schmidt, Rebecca; Vallombroso, Thomas; Galley; St. Johns, Elaine; Schwer, William; Yun, Steven; Beachley, William; Sanger, Warren; Dorn, Mary T.; Krause, Robert; Kreplick, Lance W.; Plantz, Scott H.; Cole, Jesse A.; Trestrail, John
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hardcover. Condizione: Very Good. Connecting readers with great books since 1972! Used books may not include companion materials, and may have some shelf wear or limited writing. We ship orders daily and Customer Service is our top priority.
A Woman at War: Marlene Dietrich Remembered (Painted Turtle)
Riva, J [Editor]; Lyles, A. C. [Contributor]; Hens, Alfred [Contributor]; Brunelin, Andre G. [Contributor]; Klarsfeld, Beate [Contributor]; Bacharach, Burt [Contributor]; cher, cher [Contributor]; Schumann, Coco [Contributor]; Oldfield, Col. Barney [Contributor]; McIntosh, Elizabeth [Contributor]; Moeller, Felix [Contributor]; Stern, Guy [Contributor]; Will, Hans Georg [Contributor]; Knef, Hildegard [Contributor]; Riva, J [Contributor]; Dolibois, John [Contributor]; Riva, Maria [Contributor]; Wolf, Markus [Contributor]; Naumann, Michael [Contributor]; Sternberg, Nicholas von [Contributor]; Clooney, Rosemary [Contributor]; Langhoff, Thomas [Contributor]; Kuehn, Volker [Contributor]; Schloendorff, Volker [Contributor]; Dawson, William F.
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Advanced Paediatric Life Support: The Practical Approach (Advanced Life Support Group)
Advanced Life Support Group; Tylee; Dawson; Hatcher; Group, Advanced Life Support; Malik; McCluskey; Stewart; Fay; Krieger, Sharon; Schmidt, Rebecca; Vallombroso, Thomas; Galley; St. Johns, Elaine; Schwer, William; Yun, Steven; Beachley, William; Sanger, Warren; Dorn, Mary T.; Krause, Robert; Kreplick, Lance W.; Plantz, Scott H.; Cole, Jesse A.; Trestrail, John
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Condizione: Very Good. Free shipping. Dispatch on all orders before 3pm same day. | SHOP & WAREHOUSE OVERSTOCK - LOWEST PRICE ONLINE! This book is in Very Good condition. | ISBN: 9780727915542 | Seller SKU: U1-S-RN-uvg_HK_22508-EV.
Altre immaginiThe Criterion: A Quarterly Review. Volume XIV [14], Number LIV [54], October 1934.
T. S. Eliot (ed.); Christopher Dawson, Stephen Spender, Dylan Thomas, A. Desmond Hawkins, Montgomery Belgion, and others (contribs.)
Lingua: Inglese
Editore: Faber & Faber, London, 1934
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- Rivista/periodico
Da: George Ong Books, New York, NY, U.S.A.George Ong Books
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Aggiungi al carrelloSoft cover. Condizione: Good. xi, 180 pp., 8vo, tan wrapper with yapp edges, textblock edges untrimmed. A literary quarterly edited by T. S. Eliot during its entire run from October 1922 until it ceased publication in January 1939 ("Perhaps one of the most influential critical reviews of its day," Miller-Price 45). Includes a po…em by Dylan Thomas, an essay by Stephen Spender on W. B. Yeats, and a lengthy letter to the editor from Eric Gill, writing from Jerusalem. Also with book reviews by D. G. Bridson, Bonamy Dobrée, Christopher Dawson, A. J. Penty, G. Scott Moncrieff, Louis MacNeice, and others. Good copy overall; wrapper a bit dust and finger-soiled and age-toned, small ink mark and small faint dampstain on upper cover; wrapper's yapp edges a little frayed with some short closed tears, as usual, spine darkened.
Aquinas: Selected Political Writings
AQUINAS, THOMAS & D'ENTREVES, A. P. (Ed & Intro) & DAWSON, J. G. (Trans)
Editore: Basil Blackwell 1954, 1954
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Aggiungi al carrelloOctavo hardcover (VG+) in d/w (VG+); all our specials have minimal description to keep listing them viable. They are at least reading copies, complete and in reasonable condition, but usually secondhand; frequently they are superior examples. Ordering more than one book may reduce your overall postage costs.
Editore: USGS, 2005
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Condizione: 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 N…orth 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, 429 pages.
Editore: USGS, 2005
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Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Condizione: 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 N…orth 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, 429 pages.
Editore: USGS, 2005
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Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Condizione: 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 N…orth 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, 429 pages.
Editore: USGS, 2005
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Condizione: 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 No…rth 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 pages.
Editore: USGS, 2005
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Condizione: 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 No…rth 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 pages.
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Voices from the Past : /Xam Bushmen and the Bleek and Lloyd Collection (The Khoisan Heritage Series)
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Da: Chapter 1, Johannesburg, GAU, SudafricaChapter 1
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Buono
EUR 25,92
EUR 25,00 spedizioneSpedito da Sudafrica a U.S.A.Quantità: 1 disponibili
Softcover. Condizione: Good. First Edition. The wraps are a little shelf rubbed. Internally, light foxing. Otherwise clean. Tightly bound. r*16/07/2024. [ak]. Our orders are shipped using tracked courier delivery services.
Biennial Report of The State Historical and Natural Histroy Society of Colorado: December 1, 1920 - November 30, 1922
Ammons, E.M.; Jeancon, J.A.; Dawson, Thomas F.; Schmoll, Hazel M.
Editore: The State and Natural History Society of Colorado, Denver, 1923
- Brossura
Da: Clausen Books, RMABA, Colorado Springs, CO, U.S.A.Clausen Books, RMABA
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Molto buono
EUR 31,28
EUR 5,16 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Aggiungi al carrelloWraps. Condizione: Very Good. Ex-library copy with usual stamps, stickers, and labels. Very clean and tight textblock with minimal edge wear. 55p. Size: 8vo - Over 7 3/4" - 9 3/4 " Tall. Ex-Library Paperback.
Altre immaginiThe Criterion: A Quarterly Review. Volume XIV [14], Number LIV [54], October 1934.
T. S. Eliot (ed.); Christopher Dawson, Stephen Spender, Dylan Thomas, A. Desmond Hawkins, Montgomery Belgion, and others (contribs.)
Lingua: Inglese
Editore: Faber & Faber, London, 1934
- Brossura
- Rivista/periodico
Da: George Ong Books, New York, NY, U.S.A.George Ong Books
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Molto buono
EUR 53,63
EUR 6,51 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Aggiungi al carrelloSoft cover. Condizione: Very Good. xi, 180 pp., 8vo, tan wrapper with yapp edges, textblock edges untrimmed. A literary quarterly edited by T. S. Eliot during its entire run from October 1922 until it ceased publication in January 1939 ("Perhaps one of the most influential critical reviews of its day," Miller-Price 45). Includes… a poem by Dylan Thomas, an essay by Stephen Spender on W. B. Yeats, and a lengthy letter to the editor from Eric Gill, writing from Jerusalem. Also with book reviews by D. G. Bridson, Bonamy Dobrée, Christopher Dawson, A. J. Penty, G. Scott Moncrieff, Louis MacNeice, and others. Very good copy overall; scattered foxing spots, wrapper a touch dust-soiled, its yapp edges a little frayed with some short closed tears, as usual.
Aquinas. Selected political writings
THOMAS AQUINO [AQUINAS] (D'ENTREVES A.P., ed. & DAWSON J.G., transl.)
Editore: Oxford, Basil Blackwell 1987, 1987
- Brossura
Da: Antiquariaat Pieter Judo (De Lezenaar), Hasselt, BelgioAntiquariaat Pieter Judo (De Lezenaar)
Contatta il venditoreVenditore con 5 stelleCondizione: Usato
EUR 25,30
EUR 19,00 spedizioneSpedito da Belgio a U.S.A.Quantità: 1 disponibili
Aggiungi al carrelloxxxvi + 100pp., 22cm., softcover, Very good, ISBN 0-631-12924-3, F65994.
Altre immagini- Brossura
Da: Rarewaves.com UK, London, Regno UnitoRarewaves.com UK
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 19,45
EUR 75,89 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Paperback. Condizione: New.
