Sidorov v a (36 resultados)

No Binding. Condición: 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. Condición: 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.

343 S., OBr., Sprache: russisch.

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.…

Hardcover. Condición: 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/Hardback. Condición: 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'.…

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.

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

Hardcover/Hardback. Condición: 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.…

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

Condición: New. This is a Brand-new US Edition. This Item may be shipped from US or any other country as we have multiple locations worldwide.

Hardcover/Hardback. Condición: Good. Uchebnik po algebre dlya 9 klassa obshcheobrazovatelnykh uchrezhdenij, podgotovlennyj pod nauchnym rukovodstvom akademika A. N. Tikhonova. Soderzhit teoreticheskie svedeniya, primery resheniya zadach s podrobnymi poyasneniyami, a takzhe raznourovnevye uprazhneniya i zanimatelnye zadaniya.…

Condición: Used. pp. 572.

Condición: New.

Condición: Used. pp. 572 Illus.

Condición: Used. pp. 572.

Condición: New. In English.

Condición: New. In English.

Hardback. Condición: New. 2002 ed. Preface Constructing nonlinear parameter-dependent mathematical models is essential in modeling in many scientific research fields. The investigation of branching (bifurcating) solutions of such equations is one of the most important aspects in the analysis of such models. The foundations of the theory of bifurca- tions for the functional equations were laid in the well known publications by AM. Lyapunov (1906) [1, vol. 4] (on equilibrium forms of rotating liq- uids) and E. Schmidt (1908) [1]. The approach proposed by them has been throughly developed and is presently known as the Lyapunov-Schmidt method (see M.M. Vainberg and V.A Trenogin [1, 2]). A valuable part in the founda- tions of the bifurcation theory belongs to A. Poincares ideas [1]. Later, to the end of proving the theorems on existence of bifurcation points, infinite-dimensional generalizations of topological and variational methods were proposed by M.A Krasnoselsky [1], M.M. Vainberg [1] and others. A great contribution to the development and applications of the bifurcation theory has been made by a number of famous 20th century pure and applied mathe- maticians (for example, see the bibliography in E. Zeidler [1]).…

Hardcover. Condición: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Paperback. Condición: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Condición: As New. Unread book in perfect condition.

Hardback. Condición: New. 2002 ed. Preface Constructing nonlinear parameter-dependent mathematical models is essential in modeling in many scientific research fields. The investigation of branching (bifurcating) solutions of such equations is one of the most important aspects in the analysis of such models. The foundations of the theory of bifurca- tions for the functional equations were laid in the well known publications by AM. Lyapunov (1906) [1, vol. 4] (on equilibrium forms of rotating liq- uids) and E. Schmidt (1908) [1]. The approach proposed by them has been throughly developed and is presently known as the Lyapunov-Schmidt method (see M.M. Vainberg and V.A Trenogin [1, 2]). A valuable part in the founda- tions of the bifurcation theory belongs to A. Poincares ideas [1]. Later, to the end of proving the theorems on existence of bifurcation points, infinite-dimensional generalizations of topological and variational methods were proposed by M.A Krasnoselsky [1], M.M. Vainberg [1] and others. A great contribution to the development and applications of the bifurcation theory has been made by a number of famous 20th century pure and applied mathe- maticians (for example, see the bibliography in E. Zeidler [1]).…

Softcover. Condición: Good. 1st Edition. 280 p.

No binding. Condición: Fair. Tsel nastoyashchej knigi - privlech vnimanie shirokikh sloev naseleniya k rybe i voobshche k produktam morya, kotorye my, bezuslovno, nedostatochno znaem. V etoj knige mozhno najti kratkie svedeniya ob osobennostyakh otdelnykh vidov promyslovykh ryb. Osobuyu chast sostavlyaet kulinarnyj razdel knigi, v kotorom chitatel oznakomitsya bolee chem s 500 retseptami vkusnykh i pitatelnykh blyud iz samykh raznoobraznykh vidov ryby i moreproduktov. Khochetsya dumat, chto eta kniga okazhetsya vesma poleznoj i dlya domashnikh khozyaek, i dlya spetsialistov-kulinarov.…

Condición: guter Zustand. F. guter Zustand, Gebrauchs- und Alterungsspuren: Einbände gering abgenutzt - Band 1 Leinen an der oberen Deckelecke und an der Rückenoberkante zerrissen, bei Band 2 gleiches an zwei kleinen Stellen - Band 2 mit kleinen Papierresten, angeklebt an der unteren Ecke der Rückseite (siehe letztes Bild) - Papier teils etwas vergilbt, aber Seiten sauber und ordentlich - Band 1 Seiten teils etwas eselsohrig limitierte Auflage in 3000 Exemplaren - Predisloviye k I i II chastyam - A. A. Sidorov. Kniga kak ob"yekt izucheniya i khudozhestvennyye elementy knigi - H. P. Kashin. znacheniye knigi v drevney Rusi. (Drevnerusskaya rukopisnaya kniga) - A. I. Nekrasov. Knigopechataniye v Rossii v XVI i XVII vekakh - Pervyy period. Nachalo knigopechataniya v Rossii - Vtoroy period. Rasprostraneniye traditsiy pervopechatnikov - Tretiy period. Izmeneniya usloviy tipografskogo truda i novyye tipy knig - V. YA. Adaryukov. Kniga grazhdanskoy pechati v XVIII veke - Glava pervaya. Kniga pervoy chetverti XVIII veka - Glava vtoraya. Kniga vtoroy chetverti XVIII veka - Glava tret'ya. Kniga vtoroy poloviny XVIII veka - A. I. Kondrat'yev. Novikovskiye izdaniya - M. A. Dobrov. Tekhnika illyustrirovannoy knigi XVIII veka Predisloviye ko II chasti - M. I. Fabrikant. Vvedeniye v izucheniye russkoy knigi XIX veka - H. F. Garelin. Russkoye nauchnoye izdatel'stvo v nachale XIX veka (Rumyantsovskaya epokha) - H. P. Kashin. Al'manakhi dvadtsatykh-sorokovykh godov - A. A. Sidorov. Iskusstvo russkoy knigi - B. YA. Adaryukov. Gravyura i litografiya v knige XIX veka - I. N. Rozanov. Kniga i lyudi v XIX veke - B. YA. Adaryukov. Portrety izdateley i khudozhnikov russkoy knigi Buchreihe: Band 1 und Band 2 Seitenanzahl: 381 und 520 Seiten mit zahlreichen Bildern Format: ca. 18 x 25,5 und 17,5 x 24,5 Leinen Deutsch.…