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Earthquake Spectra at 25 Earthquake Spectra at 25

No abstract available.
Authors
Charles C. Thiel, James E. Beavers, Jack P. Moehle, Roger D. Borcherdt, Farzad Naeim, Polat Gulkan

BSSA: Worth thinking about BSSA: Worth thinking about

The Bulletin of the Seismological Society of America (BSSA) is a powerful community project that has helped us share the information necessary to keep our field moving forward since 1911. In some ways, BSSA is much like it has always been, and each issue provides us with a collection of research that has been improved by the peer review process and copyedited, typeset, and printed to...
Authors
Andrew J. Michael

Geometry of the Nojima fault at Nojima-Hirabayashi, Japan - I. A simple damage structure inferred from borehole core permeability Geometry of the Nojima fault at Nojima-Hirabayashi, Japan - I. A simple damage structure inferred from borehole core permeability

The 1995 Kobe (Hyogo-ken Nanbu) earthquake, M = 7.2, ruptured the Nojima fault in southwest Japan. We have studied core samples taken from two scientific drillholes that crossed the fault zone SW of the epicentral region on Awaji Island. The shallower hole, drilled by the Geological Survey of Japan (GSJ), was started 75 m to the SE of the surface trace of the Nojima fault and crossed the...
Authors
David A. Lockner, Hidemi Tanaka, Hisao Ito, Ryuji Ikeda, Kentaro Omura, Hisanobu Naka

Logs of paleoseismic excavations across the Central Range Fault, Trinidad Logs of paleoseismic excavations across the Central Range Fault, Trinidad

This publication makes available maps and trench logs associated with studies of the Central Range Fault, part of the South American-Caribbean plate boundary in Trinidad. Our studies were conducted in 2001 and 2002. We mapped geomorphic features indicative of active faulting along the right-lateral, Central Range Fault, part of the South American-Caribbean plate boundary in Trinidad. We
Authors
Christopher J. Crosby, Carol S. Prentice, John Weber, Daniel Ragona

OxCal: Versatile tool for developing paleoearthquake chronologies: A primer OxCal: Versatile tool for developing paleoearthquake chronologies: A primer

Ages of paleoearthquakes (events), i.e., evidence of earthquakes inferred from the geologic record, provide a critical constraint on estimation of the seismic hazard posed by an active fault. The radiocarbon calibration program OxCal (4.0.3 and above; Bronk Ramsey 2007, 2001) provides paleoseismologists with a straightforward but rigorous means of estimating these event ages and their
Authors
J. J. Lienkaemper, C.B. Ramsey

Moderate rates of late Quaternary slip along the northwestern margin of the Basin and Range Province, Surprise Valley fault, northeastern California Moderate rates of late Quaternary slip along the northwestern margin of the Basin and Range Province, Surprise Valley fault, northeastern California

The 86-km-long Surprise Valley normal fault forms part of the active northwestern margin of the Basin and Range province in northeastern California. We use trench mapping and radiocarbon, luminescence, and tephra dating to estimate displacements and timing of the past five surface-rupturing earthquakes on the central part of the fault near Cedarville. A Bayesian OxCal analysis of timing
Authors
Stephen F. Personius, Anthony J. Crone, Michael N. Machette, Shannon Mahan, David J. Lidke

Stratigraphic controls on saltwater intrusion in the Dominguez Gap area of coastal Los Angeles Stratigraphic controls on saltwater intrusion in the Dominguez Gap area of coastal Los Angeles

The Los Angeles Basin is a densely populated coastal area that significantly depends on groundwater. A part of this groundwater supply is at risk from saltwater intrusion—the impetus for this study. High-resolution seismic-reflection data collected from the Los Angeles–Long Beach Harbor Complex have been combined with borehole geophysical and descriptive geological data from four nearby...
Authors
Brian D. Edwards, Kenneth D. Ehman, Daniel J. Ponti, Eric G. Reichard, John Tinsley, Robert J. Rosenbauer, Michael T. Land

Reassessment of probabilistic seismic hazard in the Marmara region Reassessment of probabilistic seismic hazard in the Marmara region

In 1999, the eastern coastline of the Marmara region (Turkey) witnessed increased seismic activity on the North Anatolian fault (NAF) system with two damaging earthquakes (M 7.4 Kocaeli and M 7.2 D??zce) that occurred almost three months apart. These events have reduced stress on the western segment of the NAF where it continues under the Marmara Sea. The undersea fault segments have...
Authors
Erol Kalkan, Polat Gulkan, Nazan Yilmaz, Mehmet Çelebi

Accretionary orogens through Earth history Accretionary orogens through Earth history

Accretionary orogens form at intraoceanic and continental margin convergent plate boundaries. They include the supra-subduction zone forearc, magmatic arc and back-arc components. Accretionary orogens can be grouped into retreating and advancing types, based on their kinematic framework and resulting geological character. Retreating orogens (e.g. modern western Pacific) are undergoing...
Authors
Peter A. Cawood, A. Kroner, W.J. Collins, T.M. Kusky, Walter D. Mooney, B.F. Windley

How the continents deform: The evidence from tectonic geodesy How the continents deform: The evidence from tectonic geodesy

Space geodesy now provides quantitative maps of the surface velocity field within tectonically active regions, supplying constraints on the spatial distribution of deformation, the forces that drive it, and the brittle and ductile properties of continental lithosphere. Deformation is usefully described as relative motions among elastic blocks and is block-like because major faults are...
Authors
Wayne R. Thatcher

Software for inference of dynamic ground strains and rotations and their errors from short baseline array observations of ground motions Software for inference of dynamic ground strains and rotations and their errors from short baseline array observations of ground motions

In two previous articles we presented a formulation for inferring the strains and rotations of the ground beneath a seismic array having a finite footprint. In this article we derive expressions for the error covariance matrices of the inferred strains and rotations, and we present software for the calculation of ground strains, rotations, and their variances from short baseline array...
Authors
Paul Spudich, Jon B. Fletcher
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