Scotese (56 results)
Paleozoic Biogreography of Continents Bordering the Iapetus (Pre-Caledonian) and Rheic (Pre-Hercynian) Oceans (FROM: Milwaukee Public Museum Special Publications in Biology and Geology No. 2, pp. 1-22).
A. M. Ziegler, C. R. Scotese, W. S. McKerrow, M. E. Johnson and R. K. Bambach.
Published by Milwaukee Public Museum., 1977
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
Contact seller5-star sellerNo Binding. Condition: Good. ORIGINAL Reprint/Offprint from symposium volume; no covers; owner's blind stamp; light creasing of corners of leaves; light foxing of a couple of pages; o/w in good condition. Book.
Language: English
Published by American Geophysical Union., Washington, D.C., U.S.A., 1984
- Hardcover
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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Hardcover. Condition: Very Good. HARDCOVER; ex-corporate library; in very good condition. Book.
More imagesLanguage: English
Published by Epic Comics, 1986
- Softcover
- Comic
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Add to basketPaperback: 10¼" x 6¾". Condition: Fine. 1986 Edition. © 1986: Vol 1 #7 - May 1986. Slight markings to front cover:- (original cost $1.50). Isherwood, Villamonte, Saladino & Scotese (illustrator).
More imagesLanguage: English
Published by Epic Comics, 1986
- Softcover
- Comic
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Add to basketPaperback: 10¼" x 6¾". Condition: Near Mint. 1986 Edition. © 1986: Vol 1 #7 - May 1986:- (original cost $1.50). Isherwood, Villamonte, Saladino & Scotese (illustrator).
More imagesLanguage: English
Published by Marvel Comics / New Universe, 1987
- Softcover
- Comic
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Add to basketPaperback: 10¼" x 6¾". Condition: Very Fine. 1987 Edition. © 1987: Vol 1 #13 - November 1987:- (original cost $0.75). Giffen, Colletta, Brosseau & Scotese (illustrator).
More imagesLanguage: English
Published by Marvel Comics / New Universe, 1987
- Softcover
- Comic
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Add to basketPaperback: 10¼" x 6¾". Condition: Very Fine. 1987 Edition. © 1987: Vol 1 #12 - October 1987:- (original cost $0.75). Grindberg, Mas, Bryant & Scotese (illustrator).
More imagesLanguage: English
Published by Marvel Comics / New Universe, 1987
- Softcover
- Comic
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Add to basketPaperback: 10¼" x 6¾". Condition: Very Fine. 1987 Edition. © 1987: Vol 1 #8 - June 1987:- (original cost $0.75). Isherwood, Colletta, Parker & Scotese (illustrator).
Published by USGS, Denver, CO, 1999
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Add to basketCondition: very good. from the introduction, "We interpret a Phanerozoic tectonic model of the Circum-North Pacific for the orogenic collages along the eastern margin of the North Asian Craton and the western margin of the North American Craton." softcover, 11" x 8.5", 122 pages, illustrated.
Published by The Marvel Comics Group, 1985
- Softcover
Seller: The Old Sage Bookshop, Prescott, AZ, U.S.A.The Old Sage Bookshop
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Soft cover. Condition: Fine-. Perfect-bound softcover in fine minus condition: very slight scuffing to cover; straight; tight; pages excellent. 72 pages; color illustrations. Size: 4to - over 9¾ - 12" tall. Graphic Novels.
More imagesLanguage: English
Published by Marvel Comics, 1985
- Softcover
Seller: Pistil Books Online, IOBA, Seattle, WA, U.S.A.Pistil Books Online, IOBA
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Trade Paperback. Condition: Near Fine. Book is in excellent condition with very light shelf wear only, creaseless covers and spine. Binding is solid and square, covers have sharp corners, exterior shows no other blemishes, text/interior is clean and free of marking of any kind. Color comics throughout. 70 pages. Keywords: Female…, Action Hero, Green, Hulk, She-hulk, Muscle Woman, Big Hair, Hero, Action Figure, Comic Hero.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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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 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. " DV2. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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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 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. " DV1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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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 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." DV4. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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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 Nor…th 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 pages.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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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 Nor…th 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 pages.
More imagesPublished by Fratelli Palombi Editori, Roma, 1989
- Softcover
Seller: Librería Mamut, Barcelona, B, SpainLibrería Mamut
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£ 7.06
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Add to basketCondition: Bueno. 21x28. 164. Fratelli Palombi Editori, ROMA, 1989, 168pp. Italiano.
- Softcover
Seller: libreriauniversitaria.it, Occhiobello, RO, Italylibreriauniversitaria.it
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£ 20.96
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Condition: NEW.
- Hardcover
Seller: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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£ 66.24
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Condition: New. Scotese, Christopher (illustrator).
- Hardcover
Seller: California Books, Miami, FL, U.S.A.California Books
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£ 68.27
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Condition: New. Scotese, Christopher (illustrator).
Published by A.V.E., Roma, 1941
- Softcover
Seller: LIBRERIA XODO, Torino, TO, ItalyLIBRERIA XODO
Contact seller3-star sellerIn-8°, pp. 280, numerose illustrazioni fotografiche in nero f.t., brossura editoriale. False (illustrator).
- Softcover
Seller: Biblioteca di Babele, Tarquinia, VT, ItalyBiblioteca di Babele
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Condition: BUONO USATO. IED. ITALIANO Mostra tenutasi pressoGalleria Nazionale d' Arte Moderna, Roma, 7 - 28 novembre 1989. Brossura editoriale in cartoncino flessibile lucido, copertina con bandelle, illustrata da figure a colori. Buonissimo l'aspetto interno, pagine candide e ben preservate, così i tagli, integri e puliti. Ric…co di tavole a colori e in bianco e nero, nel testo. Numero pagine 163.
- Hardcover
Seller: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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£ 74.65
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Condition: As New. Unread book in perfect condition. Scotese, Christopher (illustrator).
- Hardcover
Seller: Ria Christie Collections, Uxbridge, United KingdomRia Christie Collections
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£ 63.17
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Condition: New. In. Scotese, Christopher (illustrator).
- Softcover
Seller: Libreria Studio Bosazzi, Firenze, FI, ItalyLibreria Studio Bosazzi
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£ 8.83
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Add to basketBrossura. Condition: ottimo. Edigrafital 1992, 242pp. in-8vo, ill., bella copia.
- Hardcover
Seller: GreatBookPricesUK, Woodford Green, United KingdomGreatBookPricesUK
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£ 63.16
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Condition: New. Scotese, Christopher (illustrator).
- Hardcover
Seller: GreatBookPricesUK, Woodford Green, United KingdomGreatBookPricesUK
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£ 69.32
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Condition: As New. Unread book in perfect condition. Scotese, Christopher (illustrator).
Published by Edigrafital, TERAMO, 1992
Seller: Biblioteca di Babele, Tarquinia, VT, ItalyBiblioteca di Babele
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Add to basketCondition: BUONO USATO. ITALIANO Illustrazioni presenti nel volume. Libro usato ma in buone condizioni. Potrebbe presentare piccolissimi danni alle copertine e lievi piegature da lettura al dorso e/o piegature minime agli angoli, normali segni del tempo. La rilegatura potrebbe essere minimamente allentata ma integra e senza fogl…i sciolti e/o mancanze. Le pagine e/o i tagli potrebbero essere lievemente ingialliti con minima fioritura. La foto corrisponde al libro in vendita. Altre foto su richiesta. Numero pagine 242.
Language: English
Published by Boulder, Colorado The Geological Society of America, 2017
- Softcover
Seller: Joseph Burridge Books, Dagenham, United KingdomJoseph Burridge Books
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Soft cover. Condition: New. iv, 147 pages : illustrations (some color), maps (some colour) ; 28 cm. The fossil history of animal life in India is central to our understanding of the tectonic evolution of Gondwana, dispersal of India, its northward journey, and its collision with Asia. This book provides the only detailed overvie…w of the paleobiogeographic, tectonic, and paleoclimatic evolution of the Indian plate from Gondwana to Asia. This thorough, up-to-date volume is a must-have reference for researchers and students in Indian geology, paleontology, plate tectonics, and collision of continents.
X-Men: Mutant Massacre [Marvel Omnibus]
[Marvel] Louise Simonson, Chris Claremont, & Ann Nocenti et al. [writers]; John Romita Jr. et al. [pencilers]; Dan Green et al. [inkers]; Petra Scotese et al. [colorists]; Joe Rosen et al. [letterers]
- Hardcover
- First Edition
Seller: Capitol Hill Books, ABAA, Washington, DC, U.S.A.Capitol Hill Books, ABAA
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£ 134.24
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Condition: Near Fine. Near Fine. New York: Marvel Worldwide, 2018. First Thus, stated First Printing with full numberline. Tall octavo. 908, [44]pp. Color illustrations throughout. Illustrated dust jacket. Illustrated boards; red endpapers. Creasing to edges of dust jacket. Boards show light edgewear; binding sound and pages unm…arked. A Near Fine copy; collecting X-Factor (1986) #9-17, New Mutants (1983) #46, Thor (1966) #373-374, and others, all originally published in comic format.
- Softcover
Seller: moluna, Greven, Germanymoluna
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Condition: New.
