Neotectonics in Earthquake Evaluation

Here is a new, state-of-the-art guide for assessing earthquake sources throughout the contiguous United States. Because the relevant literature on the geological aspects of earthquake assessment has become so extensive in recent years, scientists should welcome this timely and compact group of new, useful syntheses of current knowledge addressing recent developments in the principal seismically active regions of the United States: the Pacific Coast; the western mountain area; the New Madrid area; New England; and the southeastern United States, including Charleston, South Carolina. Among the contributors are researchers who have made notable contributions to the art in their own right, making this an especially valuable new tool.
Neotectonic movement and earthquake assessment in the eastern United States
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Published:January 01, 1990
Abstract
Neotectonic movement in the United States east of the Rocky Mountains results from various superimposed intraplate adjustments related to movement in the North Atlantic Basin and glacial rebound. Some movements, such as slight southward tilt in the north from waning rebound and northward tilt of the entire region, appear aseismic. Others form a rectilinear grid pattern of zones of fractures and vertical movement and coincide with the distribution of seismicity. Most seismic source areas occur along northwest-trending fracture zones, which commonly have some right-lateral strike-slip displacement. They have broad, northeast-trending belts of rising highlands and sinking lowlands and are...
- basement
- displacements
- earthquakes
- Eastern U.S.
- engineering geology
- epicenters
- extension faults
- faults
- folds
- fracture zones
- geologic hazards
- lateral faults
- neotectonics
- rebound
- right-lateral faults
- seismic zoning
- seismicity
- seismotectonics
- stress
- strike-slip faults
- structural geology
- subsidence
- synclines
- tectonics
- tilt
- United States
- vertical movements