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.
Implications of the Meers fault on seismic potential in the central United States
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Published:January 01, 1990
Abstract
The Meers fault in southwestern Oklahoma, with a prominent scarp resulting from late Holocene surface displacement, is the best-expressed late Quaternary surface fault known to occur in a “stable” continental interior (or mid-plate) region (i.e., regions far removed from areas of high tectonic rates). The Meers fault is part of a major fault system that has not been the locus of major tectonic activity since the Paleozoic, and although recent surface displacements have been sizable, average late Quaternary rates have been low, based on a lack of geomorphic expression indicating significant cumulative displacement. Activity of the Meers fault is...
- damage
- displacements
- earthquakes
- engineering geology
- equations
- fault scarps
- faults
- geologic hazards
- ground motion
- magnitude
- Meers Fault
- neotectonics
- Oklahoma
- possibilities
- rates
- rupture
- seismotectonics
- stress drops
- structural geology
- tectonics
- United States
- central United States
- southwestern Oklahoma