Dawson christopher m (62 Ergebnisse)
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Zustand: Good. Former library copy. Pages intact with minimal writing/highlighting. The binding may be loose and creased. Dust jackets/supplements are not included. Includes library markings. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.
- Hardcover
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Zustand: Very Good. Former library copy. Pages intact with possible writing/highlighting. Binding strong with minor wear. Dust jackets/supplements may not be included. Includes library markings. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.
- Hardcover
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Zustand: Good. Former library copy. Pages intact with minimal writing/highlighting. The binding may be loose and creased. Dust jackets/supplements are not included. Includes library markings. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.
Weitere Bilder- Hardcover
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Hardcover. Zustand: Good+. 8vo 8" - 9" tall; 270 pages; 1969 Cambridge University Press. HC soundly bound in original red cloth lettered in gilt. Soundly bound; text has some mild scattered underlining in text. G+.
Verlag: J Applied Physics, 1970
- Softcover
- Magazin//Zeitschrift
Anbieter: Larry W Price Books, Portland, OR, USALarry W Price Books
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In den WarenkorbPamphlet. Zustand: Very Good. Vol 41, No 11, pp. 4493-4500, Illus, 4to, Extracted from orig vol, begins with title page, trimmed & stapled, thus is like a pamphlet, VG.
The Ultimate Silver Surfer
Lee, Stan (editor) & Tom Defalco; Ann Tonsor Zeddies; Len Wein; Keith R. A. DeCandido; James Dawson; Dave Smeds; John J. Ordover; Steve Rasnic Tem; Pierce Askegren; Christopher Golden; Jose R. Nieto; Sharman DiVono; Craig Shaw Gardner; David M. Honigsber
- Softcover
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Soft cover. Zustand: Fine. 340pp, Like new, unread copy, no reading creases, smooth spine, bagged. Dave Gibbons; John Buscema; Michael Avon Oeming; George Perez; Ron Frenz; Patrick Olliffe; Gary Frank; Steve Leialoha; Colleen Doran; Scot Eaton; Paul Ryan; Amanda Conner; Jordan Raskin; Tom Morgan; Grant Miehm; Scott McDaniel; Ern…ie Stiner; Mike Zeck. (illustrator).
Sprache: Englisch
Verlag: Cambridge University Press (Yale Classical Studies), 1st edn,, 1969
- Hardcover
- Erstausgabe
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Hardcover. Zustand: Near Fine. Dust Jacket Included. 1st Edition. 263p, hardback, VG+ in a VG+ dustwrapper (price-clipped) [0521073952].
God and the supernatural;: A catholic statement of the christian faith,
D'Arcy, M. C., Christopher Dawson, C. C. Martindale, and E. I. Watkin; Father Cuthbert (editor)
Verlag: Sheed & Ward
- Hardcover
Anbieter: ThriftBooks-Atlanta, AUSTELL, GA, USAThriftBooks-Atlanta
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In den WarenkorbHardcover. Zustand: Fair. No Jacket. Former library book; Readable copy. Pages may have considerable notes/highlighting. ~ ThriftBooks: Read More, Spend Less.
Sprache: Englisch
Verlag: Yale University Press, 1944
- Hardcover
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In den WarenkorbHardcover. Zustand: Good. No Jacket. 1st Edition. Ex-library. Call letters taped over on spine heel. Bookplate inside front cover. Embossed stamp on title page. Pocket and withdrawal slip removed from rear. Laid in at rear is "Postscript to Yale Classical Studies Vol. IX", two sheets, folded. Solid reading copy.
- Softcover
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- Softcover
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Weitere BilderVerlag: Prentice-Hall, 1970
- Softcover
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In den WarenkorbPaperback. Zustand: Very Good. First Edition. First Edition, First Printing. Not price-clipped. Published by Prentice-Hall, 1970. Octavo. Paperback. Book is very good with light shelf wear and spotting to page edges. 100% positive feedback. 30 day money back guarantee. NEXT DAY SHIPPING! Excellent customer service. Please email…with any questions. All books packed carefully and ship with free delivery confirmation/tracking. All books come with free bookmarks. Ships from Sag Harbor, New York.
- Hardcover
- Erstausgabe
Anbieter: MW Books Ltd., Galway, IrlandMW Books Ltd.
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First Edition. Price-clipped. Fine cloth copy in a near-fine, very slightly edge and dust-dulled dust-wrapper, now mylar-sleeved. Remains particularly well-preserved overall; tight, bright, clean and strong. Physical description: 263 p. ; 24 cm. Subject: Latin poetry. 1 Kg.
Monument to Saint Augustine : Essays on Some Aspects of His Thought Written in Commemoration of His 15th Centenary
D'Arcy, M. C.; Blondel, Maurice; Dawson, Christopher; Gilson, Etienne; Sherman, Jacob Holsinger (AFT)
- Softcover
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Zustand: New.
Verlag: Meridian, New York, 1957
- Softcover
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In den WarenkorbSoftcover. Zustand: Very Good. Reprint. 367pp. Mass market paperback. Ex-Center of Theological Inquiry Library with stamp and call numbers on first page and label on spine. Signature of a noted theologian on interior cover with inked underlining on about eight pages, wrappers moderately edgeworn, very good.
- Hardcover
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1st edition. Library copy. Near fine cloth copy, in a good if somewhat edge-nicked and dust-dulled dust-wrapper, now mylar-sleeved. Remains particularly and surprisingly well-preserved overall; tight, bright, clean and strong. Library marks remain. Physical Description: 263 pages ; 24 cm. Contents: 1. The Saturnian verse Thomas…Cole; 2. The Menaechmi: Roman comedy of errors Erich Segal; 3. Imperator histricus H. D. Jocelyn; 4. Nine epigrams from Pompeii David O. Ross, Jr.; 5. Obscura de re lucida carmina: science and poetry in De Rerum Natura Anne Amory; 6. Catullus 64 and the Heroic age Leo C. Curran; 7. Bacchus and the Horatian recusatio Edmund T. Silk; 8. Two Horatian proems: Carm. 1.26 and 1.32 Ross S. Kilpatrick; 9. Ovid and the law E. J. Kenney. Subjects: Classical literature; Classical literature History and criticism; Criticism, interpretation, etc; Littérature ancienne Histoire et critique 1 Kg.
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First Edition. Price-clipped. Fine cloth copy in a near-fine, very slightly edge and dust-dulled dust-wrapper, now mylar-sleeved. Remains particularly well-preserved overall; tight, bright, clean and strong. Physical description: 263 p. ; 24 cm. Subject: Latin poetry. 1 Kg.
Weitere BilderGOD AND THE SUPERNATURAL: A Catholic Statement of the Christian Faith
M.C. D'Arcy, S.J., Fr. Cuthbert, O.F.M. Cap., Christopher Dawson, C.C. Dawson, S.J., and E.I. Watkin
Verlag: Sheed and Ward, New York, 1954
- Hardcover
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Hardcover. Zustand: Good. Abridged Edition. 252p. A red cloth hardcover ex-library book in original binding. Label residue and scuff marks on spine. Label, stamp, and card pocket on endpapers. Otherwise, very good condition with text clean and binding tight.
Monument to Saint Augustine : Essays on Some Aspects of His Thought Written in Commemoration of His 15th Centenary
D'Arcy, M. C.; Blondel, Maurice; Dawson, Christopher; Gilson, Etienne; Sherman, Jacob Holsinger (AFT)
- Softcover
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Zustand: As New. Unread book in perfect condition.
- Softcover
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1st edition. Library copy. Near fine cloth copy, in a good if somewhat edge-nicked and dust-dulled dust-wrapper, now mylar-sleeved. Remains particularly and surprisingly well-preserved overall; tight, bright, clean and strong. Library marks remain. Physical Description: 263 pages ; 24 cm. Contents: 1. The Saturnian verse Thomas…Cole; 2. The Menaechmi: Roman comedy of errors Erich Segal; 3. Imperator histricus H. D. Jocelyn; 4. Nine epigrams from Pompeii David O. Ross, Jr.; 5. Obscura de re lucida carmina: science and poetry in De Rerum Natura Anne Amory; 6. Catullus 64 and the Heroic age Leo C. Curran; 7. Bacchus and the Horatian recusatio Edmund T. Silk; 8. Two Horatian proems: Carm. 1.26 and 1.32 Ross S. Kilpatrick; 9. Ovid and the law E. J. Kenney. Subjects: Classical literature; Classical literature History and criticism; Criticism, interpretation, etc; Littérature ancienne Histoire et critique 1 Kg.
- Softcover
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Zustand: New. In.
God and the Supernatural: A Catholic Statement of Faith
D'Arcy, M. C., Christopher Dawson, C. C. Martindale, and E. I. Watkin; Father Cuthbert (editor)
Verlag: Sheed and Ward, New York, 1954
- Hardcover
- Erstausgabe
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In den WarenkorbHardcover. Zustand: Fine. Zustand des Schutzumschlags: Very Good. First Thus. Red cloth, spine panel lettered in black. Very slightly rubbed extrems, essentially as issued. Dust jacket is a bit toned and soiled by age, with 2 1/2" separation along upper rear flap fold, now in mylar. 2nd ptg. thus (of 1936 abridged edition). x,25…2 pp. Size: 8vo - over 7¾" - 9¾" tall. Book.
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Verlag: USGS, 2005
- Softcover
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Zustand: 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 Nort…h 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.
Verlag: USGS, 2005
- Softcover
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Zustand: 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 Nort…h 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.
Verlag: USGS, 2005
- Softcover
Anbieter: Crossroads Books, Reno, NV, USACrossroads Books
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Zustand: 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 Nort…h 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.
Verlag: USGS, 2005
- Softcover
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Zustand: 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.
Verlag: USGS, 2005
- Softcover
Anbieter: Crossroads Books, Reno, NV, USACrossroads Books
Verkäufer/-in kontaktierenVerkäufer/-in mit 5 SternenVerbandsmitglied: IOBA
Zustand: Neu
EUR 27,10
EUR 4,32 VersandVersand innerhalb von USAAnzahl: 2 verfügbar
Zustand: 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.
