James V. Warren (46 results)

Trade Paperback. Condition: Very Good. Revised Edition. 8vo - over 7¾" - 9¾" tall. Light bumps and shelf wear. Inscribed by author "To Dores Happy Trails!," signed and dated "3/25/00" inside front cover. Signed by Author(s).

Paperback. Condition: VG. Revised. 138pp. Extremities lightly rubbed & scratched. Illus. Signed & inscribed by Lee on fep. Signed and Inscribed By Author.

Hardcover. Condition: Fair. No Jacket. Missing dust jacket; Readable copy. Pages may have considerable notes/highlighting. ~ ThriftBooks: Read More, Spend Less. Frank Sieminski (illustrator).

Hardcover. Condition: 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.

Condition: Good. The book may have minor cosmetic wear like creased spine, cover, scratches, curled corners, folded pages, minor sunburn, minor water damage, minor bent. The book may have some highlights, notes, underlined pages. Accessories such as CD, codes, toys, may not be included . Safe and Secure Mailer. No Hassle Return.…

Revised edition INSCRIBED, SIGNED, AND DATED BY THE AUTHOR. 140 pages. Paperback: H 21.5cm x L 14cm. Black stiff paper covers lightly rubbed, publisher's "autographed copy" sticker affixed upon front cover. A near fine copy and inscribed "To Leroy | Happy Trails | James V. Lee | 9/11/99" on the verso of the front cover. ISBN 0966387007.…

Hardcover. Condition: Good. HARDCOVER Good - Bumped and creased book with tears to the extremities, but not affecting the text block, may have remainder mark or previous owner's name - GOOD Oversized.

Softcover. Condition: Very Good with no dust jacket. Stapled binding is tight. Pages off-white and clean with some creasing of a few pages at the beginning. Wrappers have light overall shelf wear, edge rubbing, creasing. Contents: Roberts, "Letter to the Reader"; Mitchell, "Windows of the Heart: The Letters of Margaret Roberts to Thomas Wolfe"; Clark, "Getting Dick Prosser Right"; Peterson, "Thomas Wolfe's The Child by Tiger, A Historical Allusion"; Westminster, "A Portrait of an American Artist: The Implied Author/Protagonist Relationship in Wolfe's Look Homeward, Angel"; Idol, "The Town Square in Thoams Wolfe's Writings: A Representative Look"; George, "The Play's the Thing: Catching the Conscience of Thomas Wolfe's Mannerhouse"; Roberts, "In Honor of Aldo P. Magi, Editor Emeritus"; "About the Cover: Wolfe in Copenhagen"; features, notes on contributors. 8.5" tall; 94 pages.…

hardcover. Condition: 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.

Hardcover. Condition: Good. Hardcover dj/ pub.1984/ Gd.+ condition/202 pages- The Duke University Complete Heart Treatment Program. (E53439). Book.

Soft cover. Condition: Near Fine. First Edition. xvi, 143 p. : ill. ; 22 cm. Signed by James Sakine on the inside of the front cover. Signed by Author(s).

Hardcover. Condition: Near Fine. Dust Jacket Condition: Near Fine. First Edition. First edition. Near fine in near fine dust jacket. Gold stamped cloth spine, dust jacket shows light rubs on edges, clean text.

Encuadernación de tapa dura. Condition: Muy bien. Dust Jacket Condition: Muy bien. 1ª Edición.

hardcover. Condition: New.

hardcover. Condition: New.

hardcover. Condition: New.

Hardcover. Condition: Good. Hardcover; includes three folded plates and 2 microfiche in rear pocket; ex-library; light foxing of edges; o/w in good condition. This is a heavy volume; extra shipping may be required for priority mail or international orders. Book.

Hardcover. Condition: Good. Hardcover; includes three folded plates and 2 microfiche in rear pocket; ex-corporate library; corners bumped, foxing spots on endpages and edges; o/w in good condition. This is a heavy volume; extra shipping may be required for priority mail or international orders. Book. …

Soft cover. Condition: Good. No Jacket. 6th edition ; 604 p. : ill. ; 28 cm. ; ISBN: 089145358X; 9780891453581 LCCN: 89-205042 ; LC: NK1125; Dewey: 745.1/075 ; OCLC: 15984965 ; "From A to Z, Schroeder's provides a guide to antiques with histories, background information, and original photographs. Illustrated." ; "After writing their first book, The Story of Fiesta, published in 1974, the Huxfords became pottery editors for Collector Books and in that capacity wrote several other books on various Ohio potteries: Roseville Pottery, McCoy Pottery, Brush-McCoy Pottery, Weller Pottery, and Roseville Pottery, Volume II. Since 1982 they have been editors of Schroeder's Antiques Price Guide; Schroeder's Collectible Toys; Antique to Modern; Garage Sale & Flea Market Annual; and Wanted to Buy." ; "The current values in this book should be used only as a guide. They are not intended to set prices, which vary from one section of the country to another. Auction prices as well as dealer prices vary greatly and are affected by condition as well as demand." ; Contents (Abridged): ABC Plates -- Abingdon -- Adams -- Advertising -- Advertising Cards -- Advertising Dolls -- African art -- Agata -- Akro Agate -- Alexandrite -- Alhambra China -- Amberina -- American Indian Art -- Amethyst Glass -- Animal dishes -- Antiquities -- Appliances -- Art Deco -- Art Glass Baskets -- Art Nouveau -- Arts and Crafts -- Aurene -- Austrian Ware -- Autographs -- Automobilia --- Autumn Leaf -- Aviation -- Avon --- Baccarat -- Badges -- Banks -- Barber Shop -- Barometers -- Bavaria -- Beer Cans -- Belleek -- Bennington -- Big Little Books -- Black Americana -- Blue and White -- Bottles and Flasks -- Boxes -- Bronzes -- Cambridge Glass -- Canes -- Carnival Glass -- Children's Books -- Christmas -- Clocks -- Cloisonne -- Coin operated machines -- Cut Glass -- Decanters -- Decoys -- Degenhart -- Depression Glass -- Dolls -- Doulton -- Fenton -- Fiesta -- Fishing -- FLow Blbue -- Fostoria -- Frankart -- Frankoma -- Fruit Jars -- Furniture -- Games -- Graniteware -- Hall China -- Haviland -- Homer Laughlin -- Hummel -- Inkwells -- Jewelry -- Kitchen -- Knives -- Lace -- Lamps -- Majolica -- McCoy -- Meissen -- Mettlach -- Militaria -- Molds -- Movie -- Musical Instruments -- Netsukes -- Nippon -- Noritake -- Occupied Japan -- Opalescent Glass -- Orientalia -- Pairpoint -- Paperweights -- Maxfield Parrish -- Pattern Glass -- Pens & Pencils -- Personalities -- Pewter -- Photographica -- Plastics -- Playing Cards -- Political -- Post Cards -- Posters -- Pre-Columbian Artifacts -- Prints -- Quilts -- Railroad -- Razors -- Records -- Red Wing -- Norman Rockwell -- Rockwood -- Roseville -- Royal Bayreuth -- Roycroft -- Rugs -- Russian Art -- Salt Shakers -- Satsuma -- Schlegelmilch Porcelain -- Sewing -- Shaker -- Silver -- Spoons -- Staffordshire -- Steins -- Stoneware -- Teddy Bear -- Tiffany -- Tiffin -- Tools -- Toys -- Vernon Kilns -- Warwick -- Watches -- Weapons -- Weathervanes -- Wedgewood -- Weller -- Willow Ware -- Winchester -- Wood Carvings -- World's Fair -- Wrought Iron -- Zsolnay ; ex-library ; corner clipped from cover ; else G. Book. …

Hard Cover. Condition: Very Good. No Jacket. Hardcover; ex-library; minor shelfwear w/ lightly bumped corners; o/w in very good condition. This is a heavy volume; extra shipping might be required for priority mail or international orders.

HC. Condition: Gut. Oln., 237s., in gutem Zustand, [APA33,1]., Deu 400g.

Soft cover. Condition: Good. No Jacket. 1st Edition. First Corgi Paperback Edition / Third Print (first published in 1955). Paperback copy, no dustjacket as issued. 332pp. B/w photographs. Not library copy, no inscriptions, creasing to spine, tanning to pages. (34/2).

Hardcover. Condition: Fine. Dust Jacket Condition: Fine. 1st Edition. First Printing, Hardcover, Fine In Fine Dj Priced $21.95, Signed By Editor Michael Bishop On The Title Page, Also Bygregory Benford At His Story. . Signed by Author(s).

HRD. Condition: New. New Book. Shipped from UK. Established seller since 2000.

HRD. Condition: New. New Book. Shipped from UK. Established seller since 2000.

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 North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV2. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…

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 North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…

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 North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea." DV4. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…

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 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 pages.…

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 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 pages.…