Sidorov A (97 results)

No Binding. Condition: Very Good. ORIGINAL 1968 Article, disbound from journal; no covers; light creasing of upper corner of leaves; o/w in very good condition. Journal.

Hard Cover. Condition: Very Good. No Jacket. Consultants Bureau, 1960, 4to, 119 pages. Book bound in a brown cloth, no dust jacket, Ex-Libris with the usual markings. Book very good. Size: 4to - over 9¾" - 12" tall.

Hardcover. Condition: Gut. 791 S. Buch.

343 S., OBr., Sprache: russisch.

Hardcover. Condition: Very Good. Dust Jacket Condition: Very Good. A clean unmarked copy with a lightly worn dust jacket. 180 pages.

4°, 9 S./p., 33 Abbildungen (Holzschnitte) im Anhang/illustrations (woodcut illustrations) in the appendix, 1 Porträt-Frontispiz/frontispiece, Originalleineneinband (publisher's cloth binding), Einband gering gebrauchsspurig / binding shows some tear and wear, sonst gutes Exemplar (otherwise fine), (Mastera kniznoj grafiki), Andrei Dmitrievich Goncharov, 1903-1979, Russian graphic artist and illustrator. Sprache: russisch. …

Hardcover. Ecru linen over boards with small embossed decoration and black Cyrillic lettering; 239 pp. with 60 color and bw plates and XI bw photographs. Text in Russian. With two main essays about European Masters of the 15h to 20th centuries and Masters of Russian and Soviet Art. Each of those is followed by subsequent related essays on Rembrandt, artists of the Parisian proletariat, Durer, graphics, revolution and art; Russian graphics, Goncharov, Rerberg and more. With an extensive section of plates showing paintings, sculpture, drawings, graphics, etc. and indeces. VG+ interior (as if unread) but with museum ex-lib. book plate inside front cover; boards very lightlyl warped.…

Hardcover. Condition: Very Good/No Dj. Gray paper covered boards with maroon cloth spine. Edges and corners show rubbing. Illustrated with b/w drawings. Tight copy. 392 pp. Photo on request.

leg. bross. Condition: Good. in ottavo leg. bross. pp. 80 Buono (Good) Buon es., segni del tempo. Book.

Soft cover. Condition: Very Good. 1st Edition. Paperback. Octavo. 31, [1]pp (text), [8]pp (plates). Original illustrated wrappers. Scarce exhibition catalogue with useful biographical notes on the Soviet artists, followed by 20 black and white reproductions of drawings, etchings, drypoints, lithographs, and linocuts by Vladimir Favorsky, Pavel Kirpichev, Nikolai Pavlov, Leonid Soifertis, Evgeny Charushin, Evgeny Kibrik, Sarra Shor, and Viktor Bibikov, 162 item catalogue. Covers thumbed and lightly creased. …

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.…

Folio, 12 Bl., 128 Tafeln im Anhang / plates in the appendix, 8 Bl., Originalleineneinband (publisher's cloth binding), gutes Exemplar (fine), Sprache: russisch.

Condition: new. Pages: 544 Language: Russian. Poety - vsegda nabljudateli. Poety - vsegda nakopiteli. Poety - vsegda otkryvateli. Poety - vsegda obolstiteli. Poety - vsegda zavirateli. Poety - izvechnye stranniki. Poety - ljudi propaschie. Ikh sudby kak zvezdy vskhodjaschie. I nastezh ikh dushi raspakhnuty. Ob etom i razmyshljaet avtor ocherednogo sbornika liricheskikh stikhotvorenij Anatolij Sidorov. 9785448463327.…

Hardcover. Condition: Collectible - Very Good. Dust Jacket Condition: Very Good. Hardcover with white cloth covers with gilt lettering. Some edgewear and chipping to DJ edges. 12x8.75 249 pages. DJ in brodart cover. Owners name on ffep. Some fading on DJ spine. Illustrated with b/w and color illustrations. Text in Russian.…

Hardcover. Condition: Very Good. errata slip, 654p. Original gray binding. No jacket. Russian text. Translation of title: Russian-Indian Interactions in the 18th century: a Collection of Documents.

Hardcover. Condition: As New. Dust Jacket Condition: Very Good. M. 1976/, pp. 366. Mainly 17-18th C. Early Russian printing. Articles by Luppov + others.

Hardcover/Hardback. Condition: Fair. Dannyj sbornik predstavlyaet soboj pervuyu popytku dat shirokim chitatelskim krugam vozmozhnost oznakomitsya s razvitiem russkoj ocherkovoj literatury, po-svoemu otrazivshej mnogie vazhnye protsessy i yavleniya narodnoj zhizni.Pri otbore proizvedenij dlya nastoyashchego sbornika sostaviteli stremilis pokazat, kak voznikala, a zatem vse bolee razrastalas i vidoizmenyalas russkaya ocherkovaya literatura, kakie mnogoobraznye formy ona porozhdala.Ponyatie 'ocherk' preterpevalo v khode literaturnogo razvitiya vesma sushchestvennye izmeneniya, i v ryade sluchaev okazyvaetsya vesma zatrudnitelnym ustanovit tverdye granitsy, otdelyayushchie ocherk ot drugikh raznovidnostej povestvovatelnoj prozy i publitsistiki.Poetomu sostaviteli, rukovodstvuyas ne formalnymi i chasto vesma zybkimi priznakami zhanra, a stremleniem dat chitatelyu predstavlenie o literaturnom protsesse, schitali vozmozhnym i nuzhnym vklyuchit v sbornik nekotorye 'promezhutochnye' v zhanrovom otnoshenii proizvedeniya.Naryadu s proizvedeniyami davno, malo ili vovse ne pereizdavavshimisya, v sbornik vklyucheny shiroko izvestnye ocherkovye proizvedeniya klassikov russkoj literatury s tem, chtoby chitatel imel vozmozhnost predstavit sebe bolee ili menee polnuyu kartinu putej razvitiya russkogo ocherka, kartinu tvorcheskikh iskanij i raznoobraznykh khudozhestvennykh reshenij, kotorye davali v etom zhanre pisateli razlichnykh darovanij i literaturnykh napravlenij.…

347 S., Originalhalbleinenband (publisher's halfcloth binding), gutes Exemplar (fine), Sprache: russisch.

Hardcover/Hardback. Condition: As New. Monografiya podgotovlena gruppoj issledovatelej zhurnalistiki i posvyashchena tsennostnomu, novomu i eshche malo izuchennomu, aspektu funktsionirovaniya sredstv massovoj informatsii i zhurnalistskoj deyatelnosti. Tsennostnoe izmerenie zhurnalistiki i uslovij ee vzaimodejstviya so svoej auditoriej i obshchestvom v tselom; idealy i tsennosti - kak transliruemye pressoj, tak i porozhdaemye eyu; tsennostnye aspekty truda zhurnalista; nakonets, obektivnye predposylki vozniknoveniya novogo nauchnogo napravleniya po issledovaniyu media. Eto i soderzhanie predprinyatogo izdaniya, i predstavlennye v obshchem vide kontury novoj nauchnoj distsipliny - aksiologii zhurnalistiki. Monografiya orientirovana na analitikov mediasfery, a takzhe spetsialistov drugikh oblastej obshchestvennykh nauk, v toj ili inoj mere zatragivayushchikh v svoikh issledovaniyakh mir massovoj informatsii.…

Hardcover/Hardback. Condition: Fair. Kniga predstavlyaet soboj sbornik statej pro otnosheniya Slavyan i Zapada:Literatura i iskusstvoD.D. Blagoj Moskva Nr. 'Dva stikhotvoreniya Pushkina o Georgii Chernom'Zhak Shaje Parizh Nr. 'Turgenev i Poema Shossona'A.A. Ilyushin Moskva Nr. 'O nekotorykh formakh grotesknoj obraznosti v literature i iskusstve'I.K. Gorskij Moskva Nr. 'Ob odnoj osobennosti poezii Slovatskogo'I.I. Svirida Moskva Nr. 'Inostrannye khudozhniki v Polshe konets XVIII Nr. pervaya tret XIX vekov'Tadeush Sivert Varshava Nr. 'Polskij emigrant Yan Chinskij i parizhskij teatr XIXnbsp;veke'L.N. Titova Moskva Nr. 'Lyubitelskij teatr i cheshskaya kultura XIX veke'Yu.I. Ritchik Moskva Nr. 'Shekspirovskie spektakli v prazhskom Vremennom teatre'Yuliush Stazhinskij Varshava Nr. 'Delakrua, Shopen i romanticheskij orfizm'Stefan Yarotsinskij Varshava Nr. 'Romantizm ili romantizmy?'Vitold Rudzinskij Varshava Nr. 'O znachenii i roli muzyki Stanislava Monyushko'Yuzef Khominskij Varshava. Karol Shimanovskij i zapadnoevropejskaya muzyka'L.S. Ginzburg Moskva Nr. 'Dzhuzeppe Tartini v russkoj muzykalnoj zhizni'Diter Kerner Majnts Nr. 'Praga v zhizni MotsartamJitka Snizhkova Praga Nr. 'Mnogogolosie v muzyke cheshskogo Renessansa'Jirzhi Vyslouzhil Brno Nr. 'Moravskij i slovatskij folklor kak stileobrazuyushchij element muzyki Yanachka'Aleksandr Bukhner Praga Nr. 'Oskar Nedbal vo glave venskogo Orkestra obshchestva muzykantov'IstoriyaE.P. Naumov Moskva Nr. 'Slavyanskie strany v zapadnoevropejskoj publitsistike XIVnbsp;veke'A.I. Rogov Moskva Nr. 'Polsha v russkikh istoricheskikh i geograficheskikh sochineniyakh XVIInbsp;veke'V.A. Dyakov Moskva Nr. 'Polskie konspiratory 1830Nr.1840-kh godov v ikh svyazyakh s Frantsiej'A.S. Mylnikov Leningrad Nr. 'Cheshskie zemli v osveshchenii nemetskoj pressy serediny XVIII veke'.…

Hardcover. Condition: Fair. First edition. 121p. Oversize. Ex-library hardcover book. Standard library marks and labels else a clean tight book in very good condition.

Hardcover. Greenish boards with brown spine and lettering and blind-stamp decoration. Cream dj with decorative illustration and red Cyrillic lettering. 395 pp. with 138 bw illustrations. Errata slip inserted in back. This work is the first generalized history of Russian book engravings since their appearance in Russia. The author of this volume has limited in the scope of the research to only book engraving, leaving aside landscape and other engravings. All these varieties of prints deserve their own special consideration. The book examines the relationship between painting and seal engraving and printing technique in Moscow in anonymous editions of the XVI century, along with publications of Ivan Fedorov and his immediate successors, and the woodcut in the Russian book of the XVII century. Also included are copper engravings and a summary of Russian portrait engravings of the XVII century. Text in Russian. VG- clean and tight text but with page edges yellowed to page 4; some pages still uncut; edge wear to covers. DJ worn at edges and soiled but solid.…

Band / tom X, Kniga vtoraja: Zivopis' i grafika (prodolzenie). 4°, 557 S./pp., zahlreiche Abbildungen/numerous illustrations, Originalleineneinband (publisher's cloth binding), gutes Exemplar (fine), Sprache: russisch.

Paperback. Condition: New.

Softcover/Paperback. Condition: Good. Materialy mezhdunarodnoj nauchno-prakticheskoj konferentsii 25-26 aprelya 2011 goda.

Paperback. Condition: Very Good. First Edition. Wraps. 8vo. Illustrated blue wraps. pp 32 and 20 plates. Soviet graphic art collected by VOKS (the U. S. S. R. Society for Cultural Relations with Foreign Countries). Very good.