Shallow lithological structure across the Dead Sea Transform derived from geophysical experiments

نویسندگان
چکیده

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Shallow 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 کامل

Legendre-transform structure derived from quantum theorems

S.P. Flego, A. Plastino , and A.R. Plastino 4 Universidad Nacional de La Plata, Instituto de F́ısica (IFLP-CCT-CONICET), C.C. 727, 1900 La Plata, Argentina and Universitat de les Illes Balears and IFISC-CSIC, 07122 Palma de Mallorca, Spain Universidad Nacional de La Plata, Facultad de Ingenieŕıa, Depto. de Ciencias Básicas, 1900 La Plata, Argentina 3 CREG-University of La Plata-CONICET Instituto...

متن کامل

Buckling of the Oceanic Lithosphere from Geophysical Data and Experiments

_Abstract. Two major hypotheses have been advanced for the formation of the long wavelength (100-300 km) undulations of oceanic basement and overlying sediments developed in the central Indian Ocean basin: whole layer folding (buckling) and local thickening (inverse boudinage). Using appropriately scaled two-layer analogue models for the oceanic lithosphere comprising a brittle layer above a du...

متن کامل

HF Radar Sea-echo from Shallow Water

HF radar systems are widely and routinely used for the measurement of ocean surface currents and waves. Analysis methods presently in use are based on the assumption of infinite water depth, and may therefore be inadequate close to shore where the radar echo is strongest. In this paper, we treat the situation when the radar echo is returned from ocean waves that interact with the ocean floor. S...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Geochemistry, Geophysics, Geosystems

سال: 2011

ISSN: 1525-2027

DOI: 10.1029/2011gc003678