Slip rate and locking depth from GPS profiles across the southern Dead Sea Transform
نویسندگان
چکیده
منابع مشابه
Crustal deformation along the Dead Sea Transform and the Carmel Fault inferred from 12 years of GPS measurements
[1] Large-scale crustal deformation in the Levant is mainly related to the DST and the CFS. The former is an active left lateral transform, bounding the Arabian plate and the Sinai sub-plate, and the latter branches out of the former and separates the Sinai sub-plate into two tectonic domains. In this study we obtain the velocities of 33 permanent GPS stations and 145 survey stations that were ...
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The effect of temperature on the main feeding parameters of Mnemiopsis leidyi from the southern Caspian Sea was studied in 2002. The clearance rates and daily rations were estimated from laboratory experiments in a wide range of temperatures from 12 to 27 ?C for M. leidyi of 12?17 mm in length. Clearance rate values changed from 52.5 to 107.3 ml ind-1 h-1. The coefficient Q10 in temperature 12 ...
متن کاملUncertainty in the Determination of Fault Locking Depth and Strike Slip Rates by Gnss Measurements
Original scientific paper A GNSS network of 36 points was established in 2006 in the eastern part of the North Anatolian Fault Zone, which is located between Tokat and Erzincan. GNSS measurements were made in 2006 ÷ 2008 in the Kelkit valley and these points’ velocities were calculated. This study compares GNSS velocities estimated with different datum definitions and the effects on fault locki...
متن کاملShallow architecture of the Wadi Araba fault (Dead Sea Transform) from high-resolution seismic investigations
In a high-resolution small-scale seismic experiment we investigated the shallow structure of the Wadi Araba fault (WAF), the principal fault strand of the Dead Sea Transform System between the Gulf of Aqaba/Eilat and the Dead Sea. The experiment consisted of 8 sub-parallel 1 km long seismic lines crossing the WAF. The recording station spacing was 5 m and the source point distance was 20 m. The...
متن کاملConstraints on fault slip rates of the southern California plate boundary from GPS velocity and stress inversions
Thorsten W. Becker,1,∗ Jeanne L. Hardebeck2 and Greg Anderson3 1Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego 9500 Gilman Drive, La Jolla CA 92093, USA 2United States Geological Survey, 345 Middlefield Road, MS 977, Menlo Park, CA 94025, USA 3UNAVCO, Inc., 6350 Nautilus Drive, Boulder, CO 80301, USA
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ژورنال
عنوان ژورنال: Journal of Geophysical Research
سال: 2008
ISSN: 0148-0227
DOI: 10.1029/2007jb005280