Dawson k r (89 risultati)
- Brossura
Da: Half Price Books Inc., Dallas, TX, U.S.A.Half Price Books Inc.
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Molto buono
EUR 6,67
EUR 3,05 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Paperback. Condizione: Very Good. Connecting readers with great books since 1972! Used books may not include companion materials, and may have some shelf wear or limited writing. We ship orders daily and Customer Service is our top priority. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;Ca…therine Yronwode;Greywolf Townsend (illustratore).
- Brossura
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Come nuovo
EUR 9,13
EUR 2,31 spedizioneSpedito in U.S.A.Quantità: Più di 20 disponibili
Condizione: As New. Unread book in perfect condition.
- Brossura
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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EUR 10,26
EUR 2,31 spedizioneSpedito in U.S.A.Quantità: Più di 20 disponibili
Condizione: New.
Editore: Geological Survey of Canada., 1974
Da: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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EUR 0,90
EUR 5,25 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
No Binding. Condizione: Very Good. ORIGINAL ARTICLE, disbound from Geological Survey of Canada publication; no covers; in very good condition. Journal.
- Brossura
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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EUR 20,03
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Condizione: As New. Unread book in perfect condition.
Lingua: Inglese
Editore: Edinburgh Medical Journal, 1937
- Brossura
Da: Sheila B. Amdur, Coventry, CT, U.S.A.Sheila B. Amdur
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EUR 18,01
EUR 4,81 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Soft cover. Condizione: Very Good. Written in ink on top of plain front cover, With the writers' compliments. pp 549-556 plus three plates. 2nd inscribed at top "Prof. Bloom with compliments" with W. Bloom name stamp underneath, pp 645-652 plus plates. Plain brown wraps.
- Brossura
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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EUR 20,76
EUR 2,31 spedizioneSpedito in U.S.A.Quantità: Più di 20 disponibili
Condizione: New.
Lingua: Inglese
Editore: Geological Survey of Canada, Ottawa, ON, Canada, 1951
- Brossura
Da: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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EUR 9,51
EUR 16,18 spedizioneSpedito da Canada a U.S.A.Quantità: 2 disponibili
Soft cover. Condizione: Very Good. Geological Survey of Canada Paper 51-24. 58pp, unbound. Folded chart collated to Contents. Titled envelope shows light wear. Reduced shipping may apply.
- Brossura
Da: Revaluation Books, Exeter, Regno UnitoRevaluation Books
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EUR 15,20
EUR 11,68 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 2 disponibili
Paperback. Condizione: Brand New. In Stock.
Geological Survy of Canada Bulletin 115. Chemical Analyses of Canadian Rocks, Minerals and Ores
Maxwell, J.A.; Dawson, K.R.; Tomilson, Margaret E.; Pocock, Dorothy M.E.; Tetrea
Editore: Department of Mines and Technical Surveys, Ottawa, Canada, 1965
- Rilegato
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
Condizione: Usato
EUR 13,51
EUR 4,42 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Hardcover. Condizione: Very Good with no dust jacket. Unmarked, except for short dedication and signature of author. ; Book Description; Spine has no signs of creasing. Pages are clean and not marred by notes or folds. Covers are square with minor wear. Ships Safe and Fast. Book Published without Dust Jacket.; Tables; 8vo 8" - 9…" tall; 476 pages; B0025ZNQMW; Signed by Author DH1.
- Brossura
Da: medimops, Berlin, Germaniamedimops
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Molto buono
EUR 17,74
EUR 10,00 spedizioneSpedito da Germania a U.S.A.Quantità: 1 disponibili
Condizione: very good. Gut/Very good: Buch bzw. Schutzumschlag mit wenigen Gebrauchsspuren an Einband, Schutzumschlag oder Seiten. / Describes a book or dust jacket that does show some signs of wear on either the binding, dust jacket or pages. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;…Catherine Yronwode;Greywolf Townsend (illustratore).
- Brossura
Da: GreatBookPricesUK, Woodford Green, Regno UnitoGreatBookPricesUK
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 11,24
EUR 17,51 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Condizione: New.
- Brossura
Da: GreatBookPricesUK, Woodford Green, Regno UnitoGreatBookPricesUK
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Come nuovo
EUR 12,85
EUR 17,51 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Condizione: As New. Unread book in perfect condition.
- Brossura
Da: Revaluation Books, Exeter, Regno UnitoRevaluation Books
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 19,82
EUR 11,68 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 5 disponibili
Paperback. Condizione: Brand New. 96 pages. 8.50x5.60x0.70 inches. In Stock. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;Catherine Yronwode;Greywolf Townsend (illustratore).
Lingua: Inglese
Editore: Missionary Independent Spiritual Church, Forestville CA 2015., 2015
- Brossura
- Prima edizione
Da: Hay Cinema Bookshop Limited, Hay on Wye, Regno UnitoHay Cinema Bookshop Limited
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EUR 9,26
EUR 23,35 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
1st edition. Slim 8vo. 96pp. Paperback in original pictorial brown wrapps. lettered in orange. Very good. ISBN 9780996052320 US$10. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;Catherine Yronwode;Greywolf Townsend (illustratore).
- Rilegato
Da: Revaluation Books, Exeter, Regno UnitoRevaluation Books
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 22,56
EUR 11,68 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 2 disponibili
Hardcover. Condizione: Brand New. In Stock.
- Brossura
Da: Ria Christie Collections, Uxbridge, Regno UnitoRia Christie Collections
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 20,81
EUR 13,99 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Condizione: New. In.
- Brossura
Da: Chiron Media, Wallingford, Regno UnitoChiron Media
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EUR 17,35
EUR 18,08 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 10 disponibili
PF. Condizione: New.
Editore: Department of Energy Mines and Resources, Ottawa, 1974
- Brossura
Da: Neil Williams, Bookseller, Victoria, BC, CanadaNeil Williams, Bookseller
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EUR 16,21
EUR 7,83 spedizioneSpedito da Canada a U.S.A.Quantità: 1 disponibili
Softcover. Condizione: VG in Wraps. Book and large map in envelope. 157 pp.
- Brossura
Da: Revaluation Books, Exeter, Regno UnitoRevaluation Books
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 25,03
EUR 11,68 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Paperback. Condizione: Brand New. 96 pages. 8.50x5.60x0.70 inches. In Stock. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;Catherine Yronwode;Greywolf Townsend (illustratore).
- Brossura
Da: GreatBookPricesUK, Woodford Green, Regno UnitoGreatBookPricesUK
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 20,34
EUR 17,51 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Condizione: New.
Lingua: Inglese
Editore: George Allen & Uwin, London, 1924
- Rilegato
Da: Books from the Past, Memphis, TN, U.S.A.Books from the Past
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Buono
EUR 32,42
EUR 6,03 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Hardcover. Condizione: Good. Ex-library. The cover has dark blue cloth with goldtone letters and a vignette. 190 pages; color frontispiece; 71 b/w illustrations on plates. The front endpaper has a handwritten date in pencil of 1937. The spine strip has darkened. A few pages and the text block ends have light foxing. Three plates… each have a closed tear on the bottom margin, 1 to 4 1/2 in. A diagonal bend line is on the front FEP, frontispiece, and first 24 pages. The pages have mild, musty odor. International shipping will require extra cost. Scans e-mailed upon request. A. Horace Gerrard and K. Leigh-Pemberton (illustratore).
- Rilegato
Da: Anybook.com, Lincoln, Regno UnitoAnybook.com
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Discreto
EUR 22,90
EUR 15,88 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Condizione: Fair. Volume 31. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Clean from markings. In fair condition, suitable as a study copy. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1…200grams, ISBN:044441892X.
Editore: The Clarendon Press, Oxford., 1959
- Rilegato
Da: Tiber Books, Cockeysville, MD, U.S.A.Tiber Books
Contatta il venditoreVenditore con 4 stelleCondizione: Usato - Molto buono
EUR 22,51
EUR 4,80 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Hardcover. Condizione: Very Good. 8vo, hardcover. No dj, blue-black cloth. Vg condition. Prev. Owner (noted molecular biologist Sol Spiegelman) name-stamp on front endpapers and textblock edges, no other marking or writing. Binding sturdy, no cover wear. 299 pp.
- Brossura
Da: GreatBookPricesUK, Woodford Green, Regno UnitoGreatBookPricesUK
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Come nuovo
EUR 23,64
EUR 17,51 spedizioneSpedito da Regno Unito a U.S.A.Quantità: Più di 20 disponibili
Condizione: As New. Unread book in perfect condition.
Editore: Canada. Department of Mines and Technical Surveys, Ottawa
- Brossura
Da: Burton Lysecki Books, ABAC/ILAB, Winnipeg, MB, CanadaBurton Lysecki Books, ABAC/ILAB
Contatta il venditoreVenditore con 5 stelleCondizione: Usato
EUR 18,91
EUR 21,86 spedizioneSpedito da Canada a U.S.A.Quantità: 1 disponibili
1956. (stiff paper covers) Very good. 46pp. Photographs, illustrations, map, graphs, tables, notes, bibliography. There is a previous owner's name on the top of the front cover. Book about Petrology. Publisher series: Geological Survey of Canada Bulletin 33. Locale: ; Goldfields Region--Saskatchewan. (Geology, Economic Geology,…Geological Surveys, Geology, Mineral Resources, Mining Industry, Mining, Gold).
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 36,92
EUR 4,42 spedizioneSpedito in U.S.A.Quantità: 3 disponibili
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, 429 pages.
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 36,92
EUR 4,42 spedizioneSpedito in U.S.A.Quantità: 2 disponibili
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, 429 pages.
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 36,92
EUR 4,42 spedizioneSpedito in U.S.A.Quantità: 3 disponibili
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, 429 pages.
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 36,92
EUR 4,42 spedizioneSpedito in U.S.A.Quantità: 7 disponibili
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 pages.
