Publications
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Effect of the northward-migrating Mendocino triple junction on the Eel River forearc basin, California: Stratigraphic development Effect of the northward-migrating Mendocino triple junction on the Eel River forearc basin, California: Stratigraphic development
The Eel River forearc basin, northern California, lies at the southern end of the Cascadia subduction zone and at the leading edge of the migrating Mendocino triple junction. Stratigraphic relationships within the Eel River forearc basin suggest that the current outer-arc high formed between ca. 3 and 2 Ma when the margin switched from a nonaccretionary to an accretionary phase and then...
Authors
Sean P. S. Gulick, Anne S. Meltzer, Samuel H. Clarke
A preliminary study on fine structures of Jiashi earthquake region and earthquake generating fault A preliminary study on fine structures of Jiashi earthquake region and earthquake generating fault
It is very unusual that nine large earthquakes of similar magnitudes (M = 6.1-6.8) occured within a very small area and a very short period of time (1997-1998) in Jiashi of Xinjiang Province, Northwest China. This paper analyzes the observed data of the aftershocks in the Jiashi earthquake region for studying the generating mechanism and deep structural background of the Jiashi strong...
Authors
S.-L. Li, X. Zhang, Walter D. Mooney, X.-L. Lai, A.J. Michael, Y.-H. Duan
32 - Rock failure and earthquakes 32 - Rock failure and earthquakes
This chapter summarizes experimental observations and related theoretical developments of faulted and intact rock properties related to earthquake nucleation, failure and dynamic slip. We will be concerned primarily with earthquakes occurring in the brittle crust. Intermediate and deep-focus earthquakes have unique mechanical considerations that are discussed in Section 7. We focus on...
Authors
David A. Lockner, Nicholas M. Beeler
35 - Strength and energetics of active fault zones 35 - Strength and energetics of active fault zones
The strength of active fault zones, i.e., the shear stress level required to cause fault slip, is fundamental to understanding the physics of earthquakes and to assessing earthquake hazard. Although many researchers have concluded that fault zones are weak (shear stresses 10 MPa or less averaged between 0 and ˜20 km depth), others maintain that faults are strong (˜100 MPa average of an...
Authors
James N. Brune, Wayne R. Thatcher
Eros: Shape, topography, and slope processes Eros: Shape, topography, and slope processes
Stereogrammetric measurement of the shape of Eros using images obtained by NEAR's Multispectral Imager provides a survey of the major topographic features and slope processes on this asteroid. This curved asteroid has radii ranging from 3.1 to 17.7 km and a volume of 2535±20 km3. The center of figure is within 52 m of the center of mass provided by the Navigation team; this minimal...
Authors
P.C. Thomas, J. Joseph, B. Carcich, J. Veverka, B.E. Clark, J.F. Bell, A.W. Byrd, R. Chomko, M. Robinson, S. Murchie, L. Prockter, A. Cheng, N. Izenberg, M. Malin, C. Chapman, L.A. McFadden, Randolph L. Kirk, M. Gaffey, P. G. Lucey
Puente Hills blind-thrust system, Los Angeles, California Puente Hills blind-thrust system, Los Angeles, California
We describe the three-dimensional geometry and Quaternary slip history of the Puente Hills blind-thrust system (PHT) using seismic reflection profiles, petroleum well data, and precisely located seismicity. The PHT generated the 1987 Whittier Narrows (moment magnitude [Mw] 6.0) earthquake and extends for more than 40 km along strike beneath the northern Los Angeles basin. The PHT...
Authors
J.H. Shaw, A. Plesch, J.F. Dolan, T. L. Pratt, P. Fiore
Processes of lithosphere evolution: New evidence on the structure of the continental crust and uppermost mantle Processes of lithosphere evolution: New evidence on the structure of the continental crust and uppermost mantle
We discuss the structure of the continental lithosphere, its physical properties, and the mechanisms that formed and modified it since the early Archean. The structure of the upper mantle and the crust is derived primarily from global and regional seismic tomography studies of Eurasia and from global and regional data on seismic anisotropy. These data as documented in the papers of this...
Authors
I.M. Artemieva, Walter D. Mooney, E. Perchuc, H. Thybo
Geomorphic studies of landslides in the Tully Valley, New York: Implications for public policy and planning Geomorphic studies of landslides in the Tully Valley, New York: Implications for public policy and planning
On April 27, 1993, a large landslide in the Tully Valley, Onondaga County, NY, destroyed three houses and resulted in the evacuation of four others; it also triggered a loss of potable drinking water for about 15 homes north of the slide area and affected a total of 20 ha of land. In the 7 years following this slide, several studies have been conducted by federal and state environmental...
Authors
D. L. Pair, W. M. Kappel
Tidal and meteorological influences on shallow marine groundwater flow in the upper Florida Keys Tidal and meteorological influences on shallow marine groundwater flow in the upper Florida Keys
No abstract available.
Authors
Christopher D. Reich, Eugene A. Shinn, Todd D. Hickey, Ann B. Tihansky
Lower crustal deformation beneath the central Transverse Ranges, southern California: Results from the Los Angeles Region Seismic Experiment Lower crustal deformation beneath the central Transverse Ranges, southern California: Results from the Los Angeles Region Seismic Experiment
We present a P wave velocity model derived from active source seismic data collected during the 1994 Los Angeles Region Seismic Experiment. Our model extends previously published upper crustal velocity models to mantle depths. Our model was developed by both ray tracing through a layered model and calculating travel times through a gridded model. It includes an 8-km-thick crustal root...
Authors
N. J. Godfrey, Gary S. Fuis, Victoria E. Langenheim, David A. Okaya, Thomas M. Brocher