Rodionov v (81 risultati)

Hardcover. Condizione: Très bon. Légères traces d'usure sur la couverture. Edition 2011. Ammareal reverse jusqu'à 15% du prix net de cet article à des organisations caritatives. ENGLISH DESCRIPTION Book Condition: Used, Very good. Slight signs of wear on the cover. Edition 2011. Ammareal gives back up to 15% of this item's net price to charity organizations.…

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

Condizione: new. Pages: 448 Language: Russian. 26 udivitelnykh istorij o pervoj ljubvi, o krepkoj druzhbe i shatkoj vrazhde, o razocharovanijakh i uspekhakh, o strogikh uchiteljakh i ljubimykh predmetakh - o shkole.A rasskazali ikh - Olga Bunina, Vladimir Vikto, Vera Vladimirova, Natalja Glazunova, Elena Dolgovesova, Elena Eremina, Olga Esaulkova, Irina Zhuk, Galina Kapustina, Ivan Kondrakov, Andrej Lobov, Jana Markova, Olga Martynova, Elena Ovchinnikova, Artak Oganesjan, Igor Rodionov, Ksenija Smirnova, Elena Smirjagina, Polina Tabagari, Ekaterina Trefilova, Dmitrij Finozhenok, Aleksandr Tsypkin, Margarita Shvetsova, Katja Shirjaeva, Elena Schetina i Anastasija Schetinina.Pochemu matematichki takie strogie? Kak vljubit v sebja glavnogo krasavchika shkoly? Chem mozhet pomoch dukh Aleksandra Kuprina na konkurse talantov? S kem pojti na bal, kogda u tebja net pary? Kak protivostojat bullingu i dat otpor nadoedlivym zadiram? 9785171809508. …

Condizione: new. Pages: 256 Language: Russian. Ne khotim tebja pugat, chitatel, no eto sbornik strashnykh rasskazov. Strashno interesnykh, strashno smeshnykh. i prosto strashnykh. Ty uzhasnjoshsja, skolko vsego mozhet sluchitsja s sovremennymi shkolnikami. No ne volnujsja: avtory podelilis etimi istorijami ne tolko chtoby poschekotat tebe nervy. Itak: kak vesti sebja, esli tebja pokhitili marsiane? chto delat, esli uchitelnitsa prevratilas v monstra - a otvechat urok vsjo ravno nado? a mozhet, tvoj zubnoj vrach okazalsja nastojaschim chudovischem? ili vdrug vyjasnilos, chto v ljubimoj entsiklopedii opisany odni lish uzhasy? kak byt, esli po sosedstvu zavelsja prizrak? Sovety po vykhodu iz etikh i mnogikh drugikh zhutkikh situatsij - v novykh kripovykh istorijakh, kotorye rasskazali: Irina Aseeva, Mara Gaag, Vera Gamajun, Aleksandr Egorov, Anna Zimova, Viktorija Medvedeva, Igor Rodionov, Valerij Ronshin, Elena Shumara i Natalja Scherba.P. S. Dlja ljubitelej bojatsja po-vzroslomu my vkljuchili v sbornik nastojaschij uzhastik: rasskaz Natali Scherby "Kotam s kljuchom v zubakh ne doverjajte". A dlja tekh, kto ljubit poveselej, tut est zabavnaja krinzhatina ot Valerija Ronshina! 9785171651190.…

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

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 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.…

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 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.…

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 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.…

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 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.…

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 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.…

Softcover/Paperback. Condizione: As New. V sbornik vklyucheny otdelnye stati avtora, posvyashchennye tvorchestvu velikogo poeta chuvashskogo naroda K. V. Ivanova Kashkra, 1890-1915. Raspolozheny v khronologicheskom poryadke.

Hardcover. Condizione: 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.

Softcover/Paperback. Condizione: Good. Vklyucheny nauchnye stati izvestnogo literaturoveda i folklorista opublikovannye v razlichnykh sbornikakh i zhurnalakh.

Softcover/Paperback. Condizione: As New. Chuvashskaya literatura1917-30-e gody. Uchebnoe posobieNa chuvashskom yazyke.

Softcover/Paperback. Condizione: As New. Chuvashskaya literatura 1917-30-e gody. Uchebnoe posobieNa chuvashskom yazyke.

Hardcover/Hardback. Condizione: Good. Traditsionnyj sbornik ostrosyuzhetnykh proizvedenij sovetskikh pisatelej.

Condizione: new. Pages: 120 Language: Russian. V uchebnike rassmotreny voprosy kompleksnogo reshenija problem intensifikatsii mjasnogo skotovodstva. Znachitelnoe mesto otvedeno voprosam effektivnogo ispolzovanija tekhnologicheskogo oborudovanija, sovershenstvovaniju tekhnologij proizvodstva produktsii mjasnogo skotovodstva, ukrepleniju kormovoj bazy, usileniju selektsionnoj raboty.Nastojaschij uchebnik prednaznachen dlja podgotovki studentov magistratury agrarnykh vysshikh uchebnykh zavedenij, obuchajuschikhsja po napravleniju podgotovki "Zootekhnija"; izdanie budet polezno aspirantam, prepodavateljam i spetsialistam, rabotajuschim v selskokhozjajstvennom proizvodstve. 9785811472253.…

Condizione: new. Pages: 140 Language: Russian. V uchebnom posobii izlozheny svedenija o biologicheskikh i khozjajstvennykh osobennostjakh krupnogo rogatogo skota, proanalizirovano sovremennoe sostojanie skotovodstva. Osoboe vnimanie udeleno tekhnologii proizvodstva moloka. Rassmotreny voprosy otsenki kachestva moloka.Prednaznacheno dlja studentov kolledzhej i tekhnikumov, obuchajuschikhsja po spetsialnostjam "Tekhnologija moloka i molochnykh produktov", "Tekhnologija proizvodstva i pererabotki selskokhozjajstvennoj produktsii", "Veterinarija", "Zootekhnija". 9785811483396.…

Hardcover/Hardback. Condizione: Good. Istoricheskoe issledovanie kandidata istoricheskikh nauk Vyacheslava Rodionova, posvyashchennoe sobytiyam Grazhdanskoj vojny na Donu i obstoyatelstvam gibeli vojskovogo atamana Donskogo kazachego vojska Alekseya Maksimovicha Kaledina. Opirayas na kontekst 1917Nr.1918 godov, avtor podvergaet somneniyu versiyu samoubijstva, vpervye rasskazyvaya o trekh pokusheniyakh na atamana i vydvigaya versiyu splanirovannogo ubijstva.…

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

Condizione: new. Pages: 320 Language: Russian. Letnij lager - eto bezopasnost, svezhij vozdukh i dobrye vozhatye. Tak dumali roditeli, sobiraja Borku i Romycha v poezdku. Vot pust i dalshe tak dumajut.Im luchshe ne znat, chto ikh deti prjatalis ot prividenija i izobretali raketu, puskali dymovukhi i borolis s mutantami. Tantsevali i rugalis. Ljubili i druzhili. Dralis i nenavideli. I stanovilis chutochku vzroslee.Vprochem, roditeli etogo i ne uznajut. Potomu chto est zakon: TO, CHTO PROISKHODIT V LAGERE - OSTAJOTSJa V LAGERE. 9785171557874.…

Condizione: New.

Condizione: New.

Condizione: New.

Condizione: New.

Condizione: New.

Condizione: As New. Unread book in perfect condition.

Condizione: As New. Unread book in perfect condition.

Buch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - This comprehensive two-volume work is devoted to the most general beginnings of mathematics. It goes back to Hausdorff's classic Set Theory (2nd ed., 1927), where set theory and the theory of functions were expounded as the fundamental parts of mathematics in such a way that there was no need for references to other sources. Along the lines of Hausdorff's initial work (1st ed., 1914), measure and integration theory is also included here as the third fundamental part of contemporary mathematics.The material about sets and numbers is placed in Volume 1 and the material about functions and measures is placed in Volume 2. Contents Fundamentals of the theory of classes, sets, and numbers Characterization of all natural models of Neumann - Bernays - Godel and Zermelo - Fraenkel set theories Local theory of sets as a foundation for category theory and its connection with the Zermelo - Fraenkel set theory Compactness theorem for generalized second-order language.…