Rodionov v (77 risultati)
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Da: Ammareal, Morangis, FranciaAmmareal
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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 p…rice to charity organizations.
Lingua: Inglese
Editore: Mir Publishers, Moscow, Mir Publishers, 1986., 1986
- Rilegato
Da: Fossilbooks, Whissonsett, NORFO, Regno UnitoFossilbooks
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EUR 12,02
EUR 24,51 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Aggiungi al carrelloHardcover. 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.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Condizione: Nuovo
EUR 27,10
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Condizione: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western N…orth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV2. softcover, wrapped in shrink wrap, tight, crisp.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
Condizione: Nuovo
EUR 27,10
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Condizione: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western N…orth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV1. softcover, wrapped in shrink wrap, tight, crisp.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
Condizione: Nuovo
EUR 27,10
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Condizione: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western N…orth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea." DV4. softcover, wrapped in shrink wrap, tight, crisp, 4.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
Condizione: Nuovo
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Condizione: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. DX1. softcover, wrapped in shrink wrap, tight, crisp, 429.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
Condizione: Nuovo
EUR 27,10
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Condizione: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. softcover, wrapped in shrink wrap, tight, crisp, 429 page.
Editore: AST, 2026
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Da: Ruslania, Helsinki, FinlandiaRuslania
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EUR 20,00
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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 Eremi…na, 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.
Lingua: Russo
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Da: Oriental Research Partners, Newtonville, MA, U.S.A.Oriental Research Partners
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EUR 23,13
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Aggiungi al carrelloSoft cover. Condizione: As New. /Mos. -Treiakovskaia. Galereia-1997/, pp. 182, ill.19th C. Russian art. [No library stamps/markings].
Editore: ChGIGN. Cheboksary. 2010, 2010
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Da: ISIA Media Verlag UG | Bukinist, Leipzig, GermaniaISIA Media Verlag UG | Bukinist
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EUR 4,40
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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.
- Rilegato
Da: Globus Books, San Francisco, CA, U.S.A.Globus Books
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EUR 33,50
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Editore: Mir Publishers, Moscow, 1986
- Rilegato
Da: Vashon Island Books, Vashon, WA, U.S.A.Vashon Island Books
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Molto buono
EUR 39,67
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Aggiungi al carrelloHardcover. 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.
Editore: Shupashkar, 2005
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Da: ISIA Media Verlag UG | Bukinist, Leipzig, GermaniaISIA Media Verlag UG | Bukinist
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Softcover/Paperback. Condizione: As New. Chuvashskaya literatura1917-30-e gody. Uchebnoe posobieNa chuvashskom yazyke.
Editore: Shupashkar, 2005
- Brossura
Da: ISIA Media Verlag UG | Bukinist, Leipzig, GermaniaISIA Media Verlag UG | Bukinist
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Softcover/Paperback. Condizione: As New. Chuvashskaya literatura 1917-30-e gody. Uchebnoe posobieNa chuvashskom yazyke.
Editore: Izd. Chuvash. univ. Cheboksary. 2006, 2006
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Da: ISIA Media Verlag UG | Bukinist, Leipzig, GermaniaISIA Media Verlag UG | Bukinist
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Aggiungi al carrelloSoftcover/Paperback. Condizione: Good. Vklyucheny nauchnye stati izvestnogo literaturoveda i folklorista opublikovannye v razlichnykh sbornikakh i zhurnalakh.
Altre immaginiEditore: Molodaya gvardiya, 1987
- Rilegato
Da: ISIA Media Verlag UG | Bukinist, Leipzig, GermaniaISIA Media Verlag UG | Bukinist
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EUR 8,80
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Aggiungi al carrelloHardcover/Hardback. Condizione: Good. Traditsionnyj sbornik ostrosyuzhetnykh proizvedenij sovetskikh pisatelej.
- Rilegato
Da: Ruslania, Helsinki, FinlandiaRuslania
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EUR 30,00
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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.Prednaznach…eno dlja studentov kolledzhej i tekhnikumov, obuchajuschikhsja po spetsialnostjam "Tekhnologija moloka i molochnykh produktov", "Tekhnologija proizvodstva i pererabotki selskokhozjajstvennoj produktsii", "Veterinarija", "Zootekhnija". 9785811483396.
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Da: Ruslania, Helsinki, FinlandiaRuslania
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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, ukre…pleniju 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.
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Hardcover. Condizione: New. In shrink wrap. Looks like an interesting title.
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Da: Ruslania, Helsinki, FinlandiaRuslania
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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. Tantseva…li 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.
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Condizione: New.
Fundamentals of Functions and Measure Theory
Mikhalev, Alexander V.; Rodionov, Timofey V.; Zakharov, Valeriy K.
Lingua: Inglese
Editore: Walter de Gruyter, 2018
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Fundamentals of Functions and Measure Theory
Mikhalev, Alexander V.; Rodionov, Timofey V.; Zakharov, Valeriy K.
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Editore: Walter de Gruyter, 2018
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Fundamentals of Functions and Measure Theory (De Gruyter Studies in Mathematics, 68/2)
Zakharov, Valeriy K.; Rodionov, Timofey V.; Mikhalev, Alexander V.
Lingua: Inglese
Editore: Walter de Gruyter, 2018
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Selected Topics in Vibrational Mechanics
Blekhman, I. I. (EDT); Blekhman, L. I. (CON); Dresig, H. (CON); Duckstein, H. (CON); Ershova, O. A. (CON); Fidlin, A. (CON); Fradkov, A. L. (CON); Grishina, S. V. (CON); Indeitsev, D. A. (CON); Jensen, J. S. (CON); Landa, P. S. (CON); Rodionov, P. (CON); Shishkina, E. (CON); Sorokin, S. V. (CON)
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Fundamentals of Functions and Measure Theory
Mikhalev, Alexander V.; Rodionov, Timofey V.; Zakharov, Valeriy K.
Lingua: Inglese
Editore: Walter de Gruyter, 2018
- Rilegato
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Come nuovo
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Selected Topics in Vibrational Mechanics
Blekhman, I. I. (EDT); Blekhman, L. I. (CON); Dresig, H. (CON); Duckstein, H. (CON); Ershova, O. A. (CON); Fidlin, A. (CON); Fradkov, A. L. (CON); Grishina, S. V. (CON); Indeitsev, D. A. (CON); Jensen, J. S. (CON); Landa, P. S. (CON); Rodionov, P. (CON); Shishkina, E. (CON); Sorokin, S. V. (CON)
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Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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