Springer basel birkhäuser basel sep 2001 (6 risultati)

Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35° (e. g. , MOLNAR and OLIVER, 1969; HUESTIS et aI. , 1973). Sn arrives as a high-frequency wave train lasting tens of seconds and up to 1 to 2 minutes. Sn velocities are typically 4. 7 km/s in stable continental and oceanic lithosphere (HUESTIS et al. , 1973) and as low as 4. 3 km/s (KADINSKY-CADE et al. , 1981) in more tectonically active regions. Lg is a complex short period guided wave consisting of high-frequency P and S energy which travels primarily in the earth's crust at frequencies typically between 0. 5 and 5 Hz. It has been modeled as higher-mode Love and Rayleigh waves as well as a sequence of multiply reflected post-critical S waves trapped in a crustal guide (BOUCHON, 1982; KENNETT, 1986; BOSTOCK and KENNETT, 1990). Lg has been observed not to propagate in oceanic or very thin continental crust (PRESS and EWING, 1952; SEARLE, 1975; ZHANG and LAY, 1995). 211 pp. Englisch.…

Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -On September 1996, the United Nations General Assembly adopted the Comprehensive Nuclear-Test-Ban Treaty (CTBT), prohibiting nuclear explosions worldwide, in all environments. The treaty calls for a global verification system, including a network of 321 monitoring stations distributed around the globe, a data communications network, an international data center (IDC), and on-site inspections to verify compliance. Seismic methods play the lead role in monitoring the CTBT. This volume concentrates on the measurement and use of surface waves in monitoring the CTBT. Surface waves have three principal applications in CTBT monitoring: to help discriminate nuclear explosions from other sources of seismic energy, to provide mathematical characterizations of the seismic energy that emanates from seismic sources, and to be used as data in inversion for the seismic velocity structure of the crust and uppermost mantle for locating small seismic events regionally. The papers in this volume fall into two general categories: the development and/or application of methods to summarize information in surface waves, and the use of these summaries to advance the art of surface-wave identification, measurement, and source characterization. These papers cut across essentially all of the major applications of surface waves to monitoring the CTBT. This volume therefore provides a general introduction to the state of research in this area and should be useful as a guide for further exploration. 243 pp. Englisch.…

Taschenbuch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35° (e. g. , MOLNAR and OLIVER, 1969; HUESTIS et aI. , 1973). Sn arrives as a high-frequency wave train lasting tens of seconds and up to 1 to 2 minutes. Sn velocities are typically 4. 7 km/s in stable continental and oceanic lithosphere (HUESTIS et al. , 1973) and as low as 4. 3 km/s (KADINSKY-CADE et al. , 1981) in more tectonically active regions. Lg is a complex short period guided wave consisting of high-frequency P and S energy which travels primarily in the earth's crust at frequencies typically between 0. 5 and 5 Hz. It has been modeled as higher-mode Love and Rayleigh waves as well as a sequence of multiply reflected post-critical S waves trapped in a crustal guide (BOUCHON, 1982; KENNETT, 1986; BOSTOCK and KENNETT, 1990). Lg has been observed not to propagate in oceanic or very thin continental crust (PRESS and EWING, 1952; SEARLE, 1975; ZHANG and LAY, 1995). 232 pp. Englisch.…

Buch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -A collection of articles summarizing the state of knowledge in a large portion of modern homotopy theory. This welcome reference for many new results and recent methods is addressed to all mathematicians interested in homotopy theory and in geometric aspects of group theory. 283 pp. Englisch.…

Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Die Forderung nach einer transdisziplinären Forschung klingt plausibel und wird schnell erhoben, aber bei der konkreten Umsetzung ergeben sich eine Reihe von Problemen. Die vorliegende Studie widmet sich ausführlich der Frage, wie transdisziplinär geforscht werden kann. Als Mitarbeiter der Projektleitung konnte Marc Mogalle aktiv am Forschungsprozess des Integrierten Projektes Gesellschaft I des Schwerpunktprogramms Umwelt teilnehmen und es intensiv untersuchen. Er identifiziert und analysiert acht Problembereiche: transdisziplinäre Problemdefinition und -bearbeitung, praktische Verwendung und Zusammenarbeit mit der Praxis, Evaluation der Forschung, Organisation, Zusammenarbeit zwischen den Forschenden, Führung und Anforderungen an die Mitarbeiter. In allen acht Bereichen kommt er zu dem Ergebnis: Die disziplinäre Forschung ist der transdisziplinären systematisch überlegen. Hauptanliegen der Arbeit ist es daher aufzuzeigen, wie diese Überlegenheit überwunden werden kann. Basierend auf Arbeiten aus. 344 pp. Deutsch.…

Taschenbuch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Die Forderung nach einer transdisziplinären Forschung klingt plausibelund wird schnell erhoben, aber bei der konkreten Umsetzung ergeben sicheine Reihe von Problemen. Die vorliegende Studie widmet sich ausführlichder Frage, wie transdisziplinär geforscht werden kann. Als Mitarbeiterder Projektleitung konnte Marc Mogalle aktiv am Forschungsprozess desIntegrierten Projektes Gesellschaft I des Schwerpunktprogramms Umweltteilnehmen und es intensiv untersuchen. Er identifiziert und analysiertacht Problembereiche: transdisziplinäre Problemdefinition undbearbeitung, praktische Verwendung und Zusammenarbeit mit der PraxisEvaluation der Forschung, Organisation, Zusammenarbeit zwischen denForschenden, Führung und Anforderungen an die Mitarbeiter. In allen achtBereichen kommt er zu dem Ergebnis: Die disziplinäre Forschung ist dertransdisziplinären systematisch überlegen.Hauptanliegen der Arbeit ist es daher aufzuzeigen, wie dieseÜberlegenheit überwunden werden kann. Basierend auf Arbeiten aus.Springer Nature c/o IBS, Benzstrasse 21, 48619 Heek 360 pp. Deutsch.…