Rodionov A (77 results)

Paperback. Condition: Very Good-. Dust Jacket Condition: No Dust Jacket As Issued. Slight edge wear, with one 1" closed tear on side edge of cover. Filled with photos of Moscow in the late 1960's. ; Large 8vo 9" - 10" tall; Unpaginated pages.

Hardcover. Condition: Fine. HARDBACK original printed pictorial boards pages: 309 [iii] many text-figs. 122mm x 198mm (4.75 x 7.75") spine very slightly faded.

Soft cover. Condition: Fine. No Jacket. 4th Edition. 136 pages : illustrations (chiefly color) ; 26 cm ISBN 9785938931718, 5938931711 OCLC 57592624 LCCN 2008479507 LC ND681 .G675 2006 ; color photographic stiff paper wrappers ; Very good quality color reproductions (all plates are color) of many of the masterpieces of the Tretyakov collections --Goodreads ; FINE. Book.…

Condition: Fair. Acceptable condition. Russian edition. (Russian Theater, Books in Russian) A readable, intact copy that may have noticeable tears and wear to the spine. All pages of text are present, but they may include extensive notes and highlighting or be heavily stained. Includes reading copy only books.…

Tapa blanda. Condition: Bueno. edicion julio 1933 sin la cubierta original, version castellana de Ventura Bagues, 61 paginas, buenas condiciones de lectura.

273 p 20 cm Traducción del ruso Tatiana Enco de Valero y José María Quiroga Plá. Encuadernación editorial en rústica con huellas de uso en la cubierta. Estado de conservación: Regular.

220 S./pp., Originalbroschur (publisher's paper covers), gutes Exemplar (fine), Sprache: russisch.

Condition: Fair / Aceptable. Madrid: Ed. España, 1930.- 273 p.; 8º mayor (19,2 x 12,9 cm); Rústica Ed. ilustrada. Ligeramente fatigado. Libro en español LITERATURA Y ESTUDIOS LITERARIOS EXTRANJEROS DE LOS SIGLOS XVI-XXI.

Soft cover. Condition: Good. Good for year, paperback. Generally clean, bright and tight. Some marks and age tanning but otherwise in good condition.

Soft cover. Condition: As New. /Mos. -Treiakovskaia. Galereia-1997/, pp. 182, ill.19th C. Russian art. [No library stamps/markings].

Condition: new. Pages: 496 Language: Russian. Istoricheskij roman znamenitogo altajskogo pisatelja Aleksandra Mikhajlovicha Rodionova (1945-2013) sozdavalsja avtorom na protjazhenii dvadtsati let, vykhodil po chastjam s 1994 goda, a polnostju uvidel svet lish v 2007 godu. Glavnyj geroj romana - knjaz Matvej Petrovich Gagarin, naznachennyj v 1711 godu gubernatorom Sibiri i kaznjonnyj Petrom I v 1721 godu po tselomu rjadu tjazhkikh obvinenij. V osnove sjuzheta lezhit velikaja petrovskaja avantjura po dobyche dragotsennogo metalla vo vladenijakh dzhungarskogo khana na reke Erket, kotoraja polozhila nachalo zolotodobychi na prostorakh Sibiri. Sredi dejstvujuschikh lits pokazany realnye personazhi togo vremeni: svetlejshij knjaz Menshikov, podpolkovnik Bukholts, knjaz Bekovich-Cherkasskij i mnogie drugie. Na osnove realnykh faktov i arkhivnykh dokumentov avtor vossozdaet panoramnuju kartinu osvoenija novykh zemel i razvitija russkoj tsivilizatsii na Altae v pervoj treti XVIII veka. 9785448451072. …

Condition: new. Pages: 400 Language: Russian. Istoricheskij roman znamenitogo altajskogo pisatelja Aleksandra Mikhajlovicha Rodionova (1945-2013) sozdavalsja avtorom na protjazhenii dvadtsati let, vykhodil po chastjam s 1994 goda, a polnostju uvidel svet lish v 2007 godu. Glavnyj geroj romana - knjaz Matvej Petrovich Gagarin, naznachennyj v 1711 godu gubernatorom Sibiri i kaznennyj Petrom I v 1721 godu po tselomu rjadu tjazhkikh obvinenij. V osnove sjuzheta lezhit velikaja petrovskaja avantjura po dobyche dragotsennogo metalla vo vladenijakh dzhungarskogo khana na reke Erket, kotoraja polozhila nachalo zolotodobychi na prostorakh Sibiri. Sredi dejstvujuschikh lits pokazany realnye personazhi togo vremeni: svetlejshij knjaz Menshikov, podpolkovnik Bukholts, knjaz Bekovich-Cherkasskij i mnogie drugie. Na osnove realnykh faktov i arkhivnykh dokumentov avtor vossozdaet panoramnuju kartinu osvoenija novykh zemel i razvitija russkoj tsivilizatsii na Altae v pervoj treti XVIII veka. 9785448451676. …

Softcover/Paperback. Condition: Good. Nauchnyj zhurnal Kunstkamera. Etnograficheskie tetradi predstavlyaet soboj izdanie, posvyashchennoe izucheniyu kultur raznykh narodov. Stati zhurnala okhvatyvayut voprosy kultury, istorii i etnografii razlichnykh regionov mira.

Condition: 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.…

Condition: 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.…

Condition: 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.…

Condition: 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.…

Condition: 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.…

20x14. 61 pags. Cub. de Mauricio Amster. Trad. Ventura Bagues.

Hardcover. Condition: Very Good. No Dust Jacket. Revised Edition. In pictorial glossy boards, 8vo, 308pp. A scarce Russian publication about Bees. Text in English. Size: 8vo - over 7¾" - 9¾". Book.

Hardcover/Hardback. Condition: Good. M. Bulgakov - Sobache serdtse.A. Vanyukov - Russkie povesti trudnoj sudby: 1920-e gody.I. Volnov - Vstrecha.S. Sergeev-Tsenskij - Zhestokost.A. Tarasov-Rodionov - Shokolad.B. Pilnyak - Povest nepogashennoj luny.S. Malashkin - Luna s pravoj storony, ili neobyknovennaya lyubov.…

Hardcover/Hardback. Condition: Good. Sbornik statej po istorii ekonomicheskogo, sotsialnogo i politicheskogo razvitiya Udmurtii, okhvatyvayushchij razlichnye aspekty i periody vremeni, primenyayutsya printsipy marksistskogo istoricheskogo poznaniya, osveshchayutsya rol i uroven razvitiya krestyanstva na razlichnykh etapakh istorii.…

Softcover/Paperback. Condition: As New. V sbornike predstavleny tri nebolshikh proizvedeniya russkikh pisatelej P. N. Krasnova, F. D. Kryukova i I. A. Rodionova, posvyashchennye nachalnomu etapu Grazhdanskoj vojny v Rossii i peredayushchie dramatizm epokhi glazami ochevidtsev i uchastnikov sobytij.

Hardcover. Condition: Very Good. No Jacket. May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less.

Hardcover/Hardback. Condition: Good. M.Bulgakov - Sobache serdtseA.Vanyukov - Russkie povesti trudnoj sudby: 1920-e godyI.Volnov - VstrechaS.Sergeev-Tsenskij - ZhestokostA.Tarasov-Rodionov - ShokoladB.Pilnyak - Povest nepogashennoj lunyS.Malashkin - Luna s pravoj storony, ili neobyknovennaya lyubov.

Hardcover/Hardback. Condition: Good. Kniga posvyashchena issledovaniyu zarubezhnykh svyazej Udmurtii v XIXNr.XX vekakh. Avtor analiziruet vzaimodejstvie Udmurtii s razlichnymi stranami i regionami mira v etot period, vklyuchaya momenty kulturnogo, politicheskogo i ekonomicheskogo obmena.

tapa blanda. Condition: Bien. Literatura.(82) España. 1930. 19 cm. 265 p. Encuadernación en tapa blanda de editorial ilustrada. Cubierta deslucida. (=3630239=) VA189.

Hardcover. Condition: New. In shrink wrap. Looks like an interesting title.

Hardcover. Condition: Very Good. 2010 Woodhead Publishing hardcover edition. Light reading wear else very good condition.

Taschenbuch. Condition: Neu. Innovations in Digital Economy | First International Conference, SPBPU IDE 2019, St. Petersburg, Russia, October 24-25, 2019, Revised Selected Papers | Dmitrii Rodionov (u. a.) | Taschenbuch | Communications in Computer and Information Science | x | Englisch | 2020 | Springer | EAN 9783030600792 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.…