Koch D K (66 results)

Condition: As New. Unread book in perfect condition.

Condition: New.

ISBN 3-8237-5550-1 448 S 23,5x16,5cm, illustr. Hardcover, Fotos und Abbildungen im Text, gutes Exemplar.

Condition: good. A copy that has been read, remains in good condition. All pages are intact, and the cover is intact. The spine and cover show signs of wear. Pages can include notes and highlighting and show signs of wear, and the copy can include "From the library of" labels or previous owner inscriptions. 100% GUARANTEE! Shipped with delivery confirmation, if you're not satisfied with purchase please return item! Ships via media mail.…

Softcover. Condition: Very Good. First edition. Small quarto. Wrappers. xvi, 787-1023pp. Tear in gutter of preliminary page, scattered foxing on pages, spine age-toned and creased, about very good. Featuring "Uncle Remus and the Ubiquitous Rabbit" by Louis D. Rubin, Jr.; "An Interview with William Styron" by Ben Forkner and Gilbert Schricke. Poetry by Wendell Berry entitled *Song*; *The Cold Pane*; *Goods*; *A Dance*; and *A Purification*. Contributions by Louis D. Rubin, Jr., William Bedford Clark, William C. Havard, William F. Steirer, Jr., Jerry H. Bryant, Speer Morgan, Richard P. Adams, Andre Malraux, Max Webb, Edwin Mims, Donald Davidson, Ben Forkner, Gilbert Schricke, Wendell Berry, Thomas H. Landess, Pinkie, Gordon Lane, Kathryn Stripling, Frank Manley, Van K. Brock, Claude Koch, Larry Rubin, Michael Cass, Louis Dollarhide, and Ingrid Smith.…

paperback. Condition: Very Good. Rowman and Littlefield Publishers; Lanham, 2006. Trade paperback. A Very Good, binding sturdy and intact, some handling/scuff marks to covers, bit of cover edge/corner wear, scuff marks and scattered foxing to text block edges, bottom front cover corner and bottom corner of first 56 pages slightly bent, a nice, clean and unmarked copy in wraps. 8vo[octavo or approx. 6 x 9], 596pp., appendix. We pack securely and ship daily w/delivery confirmation on every book. The picture on the listing page is of the actual book for sale. Additional Scan(s) are available for any item, please inquire.Please note: Oversized books/sets MAY require additional postage then what is quoted for 2.2lb book.…

Condition: Very Good. No Jacket. 1st Edition. Nice clean bright tight book 844 pages.

15 x 21 cm, 54 S., Broschur, leicht berieben und mit minimalen Randläsuren, Ecken leicht bestoßen, wenige Marginalien.

Condition: New.

Condition: New.

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.…

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.…

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, 4.…

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.…

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 page.…

Soft cover. Condition: New. Language:Chinese.Author:DUO LUO BU SHI KE KE (Doro Bush Koch).Binding:Soft cover.Publisher:of Phoenix Publishing Media Group. Yilin Press; 1.

Condition: New.

paperback. Condition: New. In shrink wrap. Looks like an interesting title.

Condition: New. In English.

Condition: New. &Uumlber den AutorSusan Blackmore is a freelance writer, lecturer and broadcaster, and a visiting professor at the University of Plymouth. She has a degree in psychology and physiology from Oxford University (1973) an MSc and a PhD in p.

Hardcover. Condition: Fair. Withdrawn library book with usual stickers and markings. 1995 Edition. Oversize blue hardcover. Moderate shelf wear to covers and edges. Pages are unmarked.

Hardcover. Condition: VHG+. Black cloth spine, yellowish boards with inset illustration on front board. xix, 411 pages : profuse color illustrations. Contents: Preface / Michael A. Keller -- Foreword / Roberto G. Trujillo -- Introduction : from a printer's point of view / Peter Rutledge Koch -- The books of Joseph Goldyne / Robert Bringhurst -- Artists' books : some remarks on a legacy of problems / Joseph Goldyne -- Colleagues and working relationships / Joseph Goldyne -- Proofing with Joseph Goldyne at Katherine Lincoln Press / Kay Bradner -- Matching the artist's hand : a Boston-West Coast partnership / Robert Townsend -- Collaboration : images and calligraphy / Thomas Ingmire -- Notes to the catalogue raisonné -- Presses and printers -- Binderies and binders -- Catalogue raisonné -- Limited-edition books -- Unique books -- Limited-edition portfolios -- Unique portfolios -- Unique sheets of calligraphy with prints -- Alphabetical index -- Chronological index -- Printmaking terms -- Illustrations -- Author biographies -- Selected public collections -- Index -- Colophon. "This catalogue is produced in conjunction with the exhibition, Joseph Goldyne: Books, Prints & Proofs presented at the Stanford University Libraries, September 14, 2015-January 31, 2016 . Copies of Joseph Goldyne's limited-edition artists' books and portfolios, as well as a selection of preparatory drawings and prints related to his artists' books, portfolios, and calligraphy sheets are in the Joseph R. Goldyne Collection, Special Collections and University Archives, Stanford University Libraries, Stanford, California".…

Condition: New.

Gross-8°. XI, 197 S. mit 266 Abbildungen im Text u. auf 101 Tafeln. Original-Broschur. Vortitel gestempelt "Kreiskrankenhaus Bad Doberan .". -Schnitt u. Umschlag ein wenig gebräunt, leicht angestaubt u. teils ein wenig bestossen, ansonsten sauber. (Beihefte zur Zeitschrift Psychiatrie, Neurologie und medizinische Psychologie. Herausgegeben von D. Müller-Hegemann. Heft 10/11).…

Condition: New. pp. 848 Index.

Paperback. Condition: Brand New. 844 pages. 10.00x7.00x1.68 inches. In Stock.

Soft cover. Condition: New. Language:Chinese.Author:LI CHA DE KE KE (Richard Koch).Binding:Soft cover.Publisher:China Social Sciences Press; 1 (February 1. 2005).

Hardcover. Condition: Very Good. 2020 Springer hardcover edition. Light reading wear else very good condition. Contents: 1 Reflexive and Reflective Auditory Feedback, Jens Blauert, Guy J. Brown; 2 Auditory Gestalt Rules and Their Application, Sarinah Sutojo, Joachim Thiemann, Armin Kohlrausch, Steven van de Par; 3 Selective Binaural Attention and Attention Switching, Janina Fels, Josefa Oberem, Iring Koch; 4 Blackboard Systems for Cognitive Audition, Christopher Schymura, Dorothea Kolossa; 5 Formation of Three-Dimensional Auditory Space, Piotr Majdak, Robert Baumgartner, Claudia Jenny; 6 Biological Aspects of Perceptual Space Formation, Michael Pecka, Christian Leibold, Benedikt Grothe; 7 Auditory Spatial Impression in Concert Halls, Tapio Lokki, Jukka Patynen; 8 Auditory Room Learning and Adaptation to Sound Reflections, Bernhard U. Seeber, Samuel Clapp; 9 Room Effect on Musicians' Performance, Malte Kob, Sebastia V. Amengual Gari, Zora Scharer Kalkandjiev; 10 Binaural Modeling from an Evolving-Habitat Perspective, Jonas Braasch; 11 Psychophysical Models of Sound Localisation with Audiovisual Interactions, Catarina Mendonca; 12 Cross-Modal and Cognitive Processes in Sound Localization, M. Torben Pastore, Yi Zhou, William A. Yost; 13 Spatial Soundscape Superposition and Multimodal Interaction, Michael Cohen, William L. Martens; 14 Binaural Evaluation of Sound Quality and Quality of Experience, Alexander Raake, Hagen Wierstorf; 15 The Language of Rooms: From Perception to Cognition to Aesthetic Judgment, Stefan Weinzierl, Steffen Lepa, Martin Thiering; 16 Modeling the Aesthetics of Audio-Scene Reproduction, John Mourjopoulos; 17 A Virtual Testbed for Binaural Agents, Jens Blauert; 18 Binaural Technology for Machine Speech Recognition and Understanding, Richard M. Stern, Anjali Menon; 19 Modeling Binaural Speech Understanding in Complex Situations, Mathieu Lavandier, Virginia Best; 20 Creating Auditory Illusions with Spatial-Audio Technologies, Rozenn Nicol; 21 Creating Auditory Illusions with Binaural Technology, Karlheinz Brandenburg, Florian Klein, Annika Neidhardt, Ulrike Sloma, Stephan Werner; 22 Toward Cognitive Usage of Binaural Displays, Yoiti Suzuki, Akio Honda, Yukio Iwaya, Makoto Ohuchi, Shuichi Sakamoto; 23 Audition as a Trigger of Head Movements, Benjamin Cohen-Lhyver, Sylvain Argentieri, Bruno Gas; 24 Intelligent Hearing Instruments-Trends and Challenges, Eleftheria Georganti, Gilles Courtois, Peter Derleth, Stefan Launer; 25 Scene-Aware Dynamic-Range Compression in Hearing Aids, Tobias May, Borys Kowalewski, Torsten Dau. …

paperback. Condition: New. Paperback. Pub Date: 2024-06 Pages: 170 Publisher: Machinery Industry Press Industrial Robot Control and Regulation Methods provides the basics of industrial robot position description. interpolation. programming and control. Through simple. application-oriented examples. the necessary programming methods are gradually introduced. Chapter 1 outlines some basic areas of robotics. Chapters 2 to 5 deal with kinematic description and programming. and Chapters 6 and 7 deal with dynamics and contro. …

Gebundene Ausgabe. Condition: Gut. Gebraucht - Gut -The NATO Special Programme Panel on Condensed Systems of Low Dimensionality began its work in 1985 at a time of considerable activity in the field. The Panel has since funded many Advanced Research Workshops, Advanced Study Institutes, Cooperative Research Grants and Research Visits across the breadth of its remit, which stretches from self-organizing organic molecules to semiconductor structures having two, one and zero dimensions. The funded activities, especially the workshops, have allowed researchers from within NATO countries to exchange ideas and work together at a period of development of the field when such interactions are most valuable. Such timely support has undoubtedly assisted the development of national programs, particularly in the countries of the alliance wishing to strengthen their science base. A closing Workshop to mark the end of the Panel's activities was organized in Marmaris, Turkey from April 23-27, 1990, with the same title as the Panel: Condensed systems of Low Dimensionality. This volume contains papers presented at that meeting, which sought to bring together chemists, physicists and engineers from across the spectrum of the Panel's activities to discuss topics of current interest in their special fields and to exchange ideas about the effects of low dimensionality. As the following pages show, this is a topic of extraordinary interest and challenge which produces entirely new scientific phenomena, and at the same time offers the possibility of novel technological applications.…