Monger w h (22 resultados)
Anatomy of North America: Thematic Geologic Portrayals of the Continent (FROM: Tectonophysics, Vol. 187, 1991, PP. 117-134 + folded plate.
Williams, Harold, Paul F. Hoffman, John F. Lewry, James W. H. Monger and Toby Rivers.
Editorial: Elsevier Publishing Company., 1991
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Librería: Eryops Books, Stephenville, TX, Estados Unidos de AmericaEryops Books
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EUR 2,63
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Añadir al carritoNo Binding. Condición: Good. ORIGINAL Reprint/Offprint of journal article; includes folded plate w/ 6 tectonic maps of North America; inscribed by Harold Williams; light creasing of corners of leaves; o/w in good condition. Journal.
Editorial: Geology, 1982
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- Revista/Periódico
Librería: Larry W Price Books, Portland, OR, Estados Unidos de AmericaLarry W Price Books
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EUR 5,26
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Añadir al carritoPamphlet. Condición: Very Good. Vol 10, No 2, pp. 70-75, Illus, 4to, Extracted from orig vol, thus begins with title page, trimmed & stapled pamphlet, else VG.
Editorial: Geological Survey of Canada Paper 67-42, 1968, 39 Pp. + Folded Map in Rear Pocket., 1968
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Librería: Eryops Books, Stephenville, TX, Estados Unidos de AmericaEryops Books
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EUR 5,30
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Añadir al carritoSoft Cover. Condición: Very Good. Softcovers; ex-corporate library; minor shelfwear w/ light creasing of corners of wraps and leaves; o/w in very good condition.
Editorial: Geological Survey of Canada Paper 68-48, 1969, 41 Pp. + Loosely-Inserted Map., 1969
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Librería: Eryops Books, Stephenville, TX, Estados Unidos de AmericaEryops Books
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EUR 7,09
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Añadir al carritoSoft Cover. Condición: Good. Softcovers; ex-corporate library; minor shelfwear w/ small creases at corners of wraps and a few leaves; small tear on lower edge of rear wrap; light glue stain on last leaf due to facing library card; o/w in good condition.
Idioma: Inglés
Editorial: Geological Survey of Canada, Ottawa, ON, Canada, 1968
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Librería: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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EUR 6,36
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Añadir al carritoSoft cover. Condición: Very Good +. Geological Survey of Canada Paper 67-42. 39pp. Folded map in rear pocket collated to Contents. Titled card wrapper is clean and without wear. Stapled binding sound. Reduced shipping may apply.
Idioma: Inglés
Editorial: Geological Survey of Canada, Ottawa, ON, Canada, 1973
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Librería: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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EUR 9,54
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Añadir al carritoSoft cover. Condición: Very Good +. Geological Survey of Canada Paper 70-33. v, 71pp. Folded map and figure in rear pocket collated to Contents. Titled card wrapper is clean and without wear. Stapled binding sound. Reduced shipping may apply.
Contributions to Canadian Paleontology (Five Papers)
B.S. Norford and Reuben J. Ross, Jr.; T.T. Uyeno; Charles A. Ross and E.W. Bamber; Charles A. Ross and J.W.H. Monger; Charles A. Ross
Idioma: Inglés
Editorial: Geological Survey of Canada, Ottawa, ON, Canada, 1978
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Librería: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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EUR 9,54
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Añadir al carritoSoft cover. Condición: Very Good. Geological Survey Bulletin 267. 75pp. Green card wrapper clean and without wear. Stapled binding sound. Papers: New species of brachiopods and trilobites from the Middle Ordovician (Whiterock) of southeastern British Columbia (Norford, Ross); Some Late Middle Devonian (Polygnathus varcus Zone) c…onodonts from central Mackenzie Valley, District of Mackenzie (Uyeno); Middle Carboniferous and Early Permian fusulinaceans from the Monkman Pass area, northeastern British Columbia ( Ross, Bamber); Carboniferous and Permian fusulinaceans from the Ominica Mountains, British Columbia (Ross, Monger); Permian fusulinaceans from the St. Elias Mountains, Yukon Territory (Ross).
Editorial: USGS, Denver, CO, 1999
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
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Condición: Usado - Bueno
EUR 14,03
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Añadir al carritoCondición: 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.
Idioma: Inglés
Editorial: Washington D.C.: American Geophysical Union, 1987
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Librería: Antiquariat Thomas Haker GmbH & Co. KG, Berlin, AlemaniaAntiquariat Thomas Haker GmbH & Co. KG
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Condición: Usado - Bueno
EUR 10,80
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Hardcover/Pappeinband. Condición: Gut. 165 pages. Good. Ex-library with usual markings. Clean pages. Cover shows mild wear. Sprache: Englisch Gewicht in Gramm: 890.
Editorial: The Geological Soceity of America, 1985
Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
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EUR 17,38
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Añadir al carritoCondición: very good. from the introduction, "This pamphlet supplements the display sheets of Transect B2. It provides (1) descriptions of terranes on the line of Transect B2, (2) comments on gravity, magnetic and heat flow data and seismicity by R. P. Riddihough, (3) description of the seismic cross-section by R. M. Clowes, (4)… bases for the compilation of Cross-section II and (5) references." DT3. pictorial envelope, dup written in marker on cover, text 20 pages stapled, Two large folded maps, scale 1:500,000.
Idioma: Inglés
Editorial: American Geophysical Union/Geological Society of America, 1987
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Librería: Anybook.com, Lincoln, Reino UnidoAnybook.com
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EUR 27,89
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Condición: Good. Volume 18. 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 good all round condition. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,850grams, ISBN:087…5905196.
Editorial: Department of Energy, Mines and Resources, 1973
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Librería: The Bookseller, Edmonton, AB, CanadaThe Bookseller
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EUR 14,63
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Añadir al carritoStapled Wraps. Condición: Very Good-. Minor shelf wear. Owner name and date on front cover. Otherwise a square, tight, unmarked book. v, 71 pp. 2 folded maps in rear pocket.
Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
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Condición: Nuevo
EUR 27,40
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Condición: 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.
Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 27,40
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Condición: 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.
Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
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Condición: Nuevo
EUR 27,40
Envío por EUR 4,37Se envía dentro de Estados Unidos de AmericaCantidad disponible: 3 disponibles
Condición: 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.
Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 27,40
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Condición: 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.
Editorial: USGS, 2005
- Tapa blanda
Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 27,40
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Condición: 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.
Idioma: Inglés
Editorial: Ottawa, Department of Energy, Mines and Resources, 1975
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Librería: Antiquariat Bookfarm, Löbnitz, AlemaniaAntiquariat Bookfarm
Contactar con el vendedorVendedor de 5 estrellasCondición: Usado - Bueno
EUR 14,25
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Añadir al carritoSoftcover. Condición: Gut. w30877 'MPX' Geological Survey of Canada. Nr. 74-47. Upper Paleozoic Rocks of the Atlin Terrane, Northwestern British Columbia and South-Central Yukon. (5 Karte + 1 Erl.) Sprache: Englisch Gewicht in Gramm: 450.
Editorial: Department of Energy, Mines and Resources, Ottawa, Canada, 1975
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Usado - Bueno
EUR 32,75
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Añadir al carritoPaperback. Condición: Very Good. Unmarked, except for enclosing envelope, which contains stamps and some scribbling. Envelope is torn and slightly damaged on one edge and some corners show wear. Book and maps are well preserved. ; 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. ; Paper - Geological Survey of Canada ; 74-47; B&W Illustrations; 4to 11" - 13" tall; 63 pages DE4.
Idioma: Inglés
Editorial: Geological Association of Canada, Vancouver, British Columbia, Canada, 2003
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Librería: Bay Used Books, Sudbury, ON, CanadaBay Used Books
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EUR 57,25
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Soft cover. Condición: Good. Moderate wear. Binding fairly tight, pages clean. Pictures available upon request.
Mesozoic Stratigraphy and Jurassic Paleontology West of Harrison Lake, Southwestern British Columbia - Bulletin 441
Arthur, Andrew John; Geological Survey of Canada; Smith, Paul L.; Monger, W.H.; Tipper, Howard W.
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- Primera edición
Librería: RareNonFiction, IOBA, Ladysmith, BC, CanadaRareNonFiction, IOBA
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Condición: Usado - Bueno
EUR 173,79
Envío por EUR 17,30Se envía de Canada a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Paperback. Condición: Very Good. First Edition. 62 pages. "This detailed study of the lithostratigraphy and biostratigraphy of the strata permits a reconstruction of much of the history of sedimentation, volcanism, plutonism, uplift and erosion during Mesozoic time in the Coast Mountains, an area commonly devoid of stratigraphic… sections with reliable fossil control. In this bulletin several fossil groups are used to date the various lithological units that can be traced into the plutonic complex." - from Preface. Two figures stored in pocket. Light wear. Minimal library markings. A quality copy.
Editorial: Government of Canada, Ottawa, 1994
- Tapa blanda
- Primera edición
Librería: RareNonFiction, IOBA, Ladysmith, BC, CanadaRareNonFiction, IOBA
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Usado - Regular
EUR 71,25
Envío por EUR 17,30Se envía de Canada a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Añadir al carritoPaperback. Condición: Fair. First Edition. 316 pages. Bibliography. Black and white plates, maps and line drawings. Heavily worn with usual library markings. Binding intact. Title page removed.
