Access the full text.
Sign up today, get DeepDyve free for 14 days.
M. Miller, Daniel Johnson, T. Dixon, R. Dokka (2001)
Refined kinematics of the Eastern California shear zone from GPS observations, 1993-1998Journal of Geophysical Research, 106
F. Cook, A. Velden, K. Hall, B. Roberts (1999)
Frozen subduction in Canada's Northwest Territories: Lithoprobe deep lithospheric reflection profiling of the western Canadian ShieldTectonics, 18
Y. Okada (1985)
Surface deformation due to shear and tensile faults in a half-spaceBulletin of the Seismological Society of America, 75
S. Beanland, M. Clark (1994)
The Owens Valley fault zone, eastern California, and surface faulting associated with the 1872 earthquake
S. McGill, K. Sieh (1993)
HOLOCENE SLIP RATE OF THE CENTRAL GARLOCK FAULT IN SOUTHEASTERN SEARLES VALLEY, CALIFORNIAJournal of Geophysical Research, 98
Richard Bennett, B. Wernicke, James Davis, P. Elosegui, J. Snow, M. Abolins, Martha House, G. Stirewalt, D. Ferrill (1997)
Global Positioning System constraints on fault slip rates in the Death Valley Region, California and NevadaGeophysical Research Letters, 24
(1994)
Fault activity map of California and adjacent areas with locations and ages of recent volcanic eruptions, California Division of Mines and Geology
Savage Savage, Lisowski Lisowski, Prescott Prescott (1990)
An apparent shear zone trending north‐northwest across the Mojave Desert into Owens Valley, eastern CaliforniaGeophys. Res. Lett., 17
D. Dong, T. Herring, R. King (1998)
Estimating regional deformation from a combination of space and terrestrial geodetic dataJournal of Geodesy, 72
Shen Shen, Dong Dong, Herring Herring, Hudnut Hudnut, Jackson Jackson, King King, McClusky McClusky, Sung Sung (1997)
Crustal deformation in Southern CaliforniaEOS, Trans. Am. Geophys. Union, 78
B. Meade, B. Hager, S. McClusky, R. Reilinger, S. Ergintav, O. Lenk, A. Barka, H. Ozener (2002)
Estimates of Seismic Potential in the Marmara Sea Region from Block Models of Secular Deformation Constrained by Global Positioning System MeasurementsBulletin of the Seismological Society of America, 92
Dixon Dixon, Miller Miller, Farina Farina, Wang Wang, Johnson Johnson (2000)
Present‐day motion of the Sierra Nevada block, and some implications for Basin and Range tectonicsTectonics, 18
Zheng‐Kang Shen, D. Dong, T. Herring, K. Hudnut, D. Jackson, R. King, S. McClusky, Li-yu Sung (1997)
Crustal deformation measured in Southern CaliforniaEos, Transactions American Geophysical Union, 78
J. Savage, M. Lisowski, W. Prescott (1990)
An apparent shear zone trending north-northwest across the Mojave Desert into Owens Valley, easternGeophysical Research Letters
J. Savage, R. Burford (1973)
Geodetic determination of relative plate motion in central CaliforniaJournal of Geophysical Research, 78
J. Sauber, W. Thatcher, S. Solomon, M. Lisowski (1994)
Geodetic slip rate for the eastern California shear zone and the recurrence time of Mojave desert earthquakesNature, 367
R. Dokka, C. Travis (1990)
Role of the Eastern California Shear Zone in accommodating Pacific‐North American Plate motionGeophysical Research Letters, 17
(1999)
GLOBK: Global Kalman Filter VLBI and GPS analysis Program V5.0, internal memorandum, MIT, Cambridge
Meade Meade, Hager Hager, Reilinger Reilinger (2001)
Estimates of seismic potential in the Marmara region from block models of secular deformation constrained by GPS measurementsBull. Seismo. Soc. Am.
(1997)
Scripps Orbit and Permanent Array Center and Southern Calitbrnia Permanent GPS Geodetic Array, in The Global Positioning System for the Geosciences
J. Savage, M. Lisowski (1998)
Viscoelastic coupling model of the San Andreas Fault along the Big Bend, southern CaliforniaJournal of Geophysical Research, 103
B. Hager, G. Lyzenga, A. Donnellan, D. Dong (1999)
Reconciling rapid strain accumulation with deep seismogenic fault planes in the Ventura Basin, CaliforniaJournal of Geophysical Research, 104
H. Ron, G. Beroza, A. Nur (2001)
Simple model explains complex faultingEos, Transactions American Geophysical Union
T. Dixon, M. Miller, F. Farina, Hongzhi Wang, Daniel Johnson (2000)
Present‐day motion of the Sierra Nevada block and some tectonic implications for the Basin and Range province, North American CordilleraTectonics, 19
Reheis Reheis, Sawyer Sawyer (1997)
Late Cenozoic history and slip rates of the Fish lake Valley, Emigrant Peak, and Deep Springs fault zones, Nevada and CaliforniaBull. Geol. Soc. Am., 109
M. Reheis, T. Sawyer (1997)
Late Cenozoic history and slip rates of the Fish Lake Valley, Emigrant Peak, and Deep Springs fault zones, Nevada and CaliforniaGeological Society of America Bulletin, 109
E. Hearn, E. Humphreys (1998)
Kinematics of the southern Walker Lane Belt and motion of the Sierra Nevada block, CaliforniaJournal of Geophysical Research, 103
S. McGill, T. Rockwell (1998)
Ages of Late Holocene earthquakes on the central Garlock fault near El Paso Peaks, CaliforniaJournal of Geophysical Research, 103
B. Souter (1998)
Comparisons of geological models to GPS observations in southern California
W. Gan, J. Svarc, J. Savage, W. Prescott (2000)
Strain accumulation across the Eastern California Shear Zone at latitude 36°30′NJournal of Geophysical Research, 105
S. McGill, K. Sieh (1991)
Surficial offsets on the Central and Eastern Garlock Fault associated with prehistoric earthquakesJournal of Geophysical Research, 96
We use Global Positioning System (GPS) data from 1993–2000 to determine horizontal velocities of 65 stations in eastern California and western Nevada between 35° and 37° N. We relate the geodetic velocities to fault slip rates using a block model that enforces path integral constraints over geologic and geodetic time scales and that includes the effects of elastic strain accumulation on faults locked to a depth of 15 km. The velocity of the Sierra Nevada block with respect to Nevada is 11.1±0.3 mm/yr, with slip partitioned across the Death Valley, (2.8±0.5 mm/yr), Panamint Valley (2.5±0.8 mm/yr), and Airport Lake/Owens Valley (5.3±0.7/4.6±0.5 mm/yr) faults. The western Mojave block rotates at 2.1±0.8°/My clockwise, with 3.7±0.7 mm/yr of left lateral motion across the western Garlock Fault. We infer 11±2 mm/yr of right lateral motion across the Mojave region of the Eastern California Shear Zone.
Geophysical Research Letters – Wiley
Published: Sep 1, 2001
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.