PaleoseismologyPaleoseismology has become an important component of seismic risk analysis, which is mandated for nuclear power plants, dams, waste repositories, and other critical structures. This book is the first in the English language to be devoted solely to paleoseismology. It summarizes the development of the field from the 1960s to the present, encompassing material that is currently widely dispersed in journal articles. * Includes a comprehensive review of the techniques currently used in paleoseismology * Emphasizes practical methods of data collection and field studies * Covers interpretation of field data based on current theory concerning fault segmentation and recurrence cycles * Contains more than 170 line drawings and 50 photographs of paleoseismic phenomena |
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Two thumbs and 8 fingers up. The most comprehensive, up to date tome on the subject. A must for anyone in the field of engineering geology.
Contents
1 | |
29 | |
SubAqueous Paleoseismology | 119 |
Paleoseismology in Extensional Tectonic Environments | 171 |
Paleoseismology of Volcanic Environments | 271 |
Paleoseismology of Compressional Tectonic Environments | 315 |
Paleoseismology of StrikeSlip Tectonic Environments | 421 |
Using LiquefactionInduced and Other SoftSediment Features for Paleoseismic Analysis | 497 |
Application of Paleoseismic Data to Seismic Hazard Assessment and Neotectonic Research | 1 |
References | 1 |
71 | |
Radiocarbon Sampling Techniques | 75 |
Field Evaluation of Liquefaction Susceptibility of Soils with High Fines Content | 77 |
603 | |
615 | |
Color Plates | 619 |
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Common terms and phrases
active analysis associated Basin block Bull California caused central changes channel Chapter colluvium coseismic created dating deformation deposits depth described dikes displacement distribution earthquake estimated et al event evidence example fault scarp fault zone field Figure fissures fold formed Geol geologic geometry geomorphic Geophys ground historic horizon indicate interpreted interval Italy Lake landslides late lateral length lines liquefaction lower magnitude marine material maximum McCalpin measured method normal faults observed occurred offset origin paleoearthquakes paleoseismic Pleistocene probability processes produced Quaternary range record recurrence region represent result rupture samples sand sediment segment seismic shaking shown shows similar slip rate slope soil stratigraphic strike-slip structures studies subduction surface Table tectonic terraces thickness thrust trench turbidites types typically unit uplift upper vertical volcanic wall wedge zone