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 Paleoseismology eBook

Paleoseismology


Imprint: Academic Press

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Paleoseismology (the study of "ancient" earthquakes) 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. Chapters, contributed by active practitioners at the forefront of paleoseismic research, cover the entire range of techniques currently used in paleoseismic reconstruction.

* Second completely updated version of a book solely devoted to paleoseismology
* Summarizes the development of the field from the 1960's to the present
* 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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Title of eBook: Paleoseismology
Release Date: 07-06-2009
Publisher: Academic Press

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Parent title Paleoseismology
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SKU 9780080919980
File size 68137
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Paleoseismology


Chapter One

Introduction to Paleoseismology

James P. McCalpin and Alan R. Nelson

1.1 The Scope of Paleoseismology

1.1.1 Definition and Objectives

Paleoseismology is the study of prehistoric earthquakes, especially their location, timing, and size. Whereas seismologists work with data recorded by instruments during earthquakes, paleoseismologists interpret geologic evidence created during individual paleoearthquakes. Paleoseismology differs from more general geologic studies of slow to rapid crustal movements during the late Cenozoic (e.g., neotectonics) in its focus on the almost instantaneous deformation of landforms and sediments during earthquakes. This focus permits study of the distribution of individual paleoearthquakes in space and over time periods of thousands or tens of thousands of years. Such long paleoseismic histories, in turn, help us understand many aspects of neotectonics, such as regional patterns of seismicity and tectonic deformation as well as the seismogenic behavior of specific faults. Paleoseismology also is part of the broader field of earthquake geology, which includes aspects of modern instrumental studies of earthquakes (seismology), tectonics and structural geology, historical surface deformation (geodesy), and the geomorphology of tectonic landscapes (tectonic geomorphology). Books by Yeats et al. (1997), Burbank and Anderson (2001), and Keller and Pinter (2002) give different perspectives on the field of paleoseismology.

The driving force behind most paleoseismic studies is society's need to assess the probability and severity of future earthquakes (Reiter, 1995; Gurpinar, 2005). In the decade sin

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