Late Cenozoic uplift along the northern Dead Sea transform in Lebanon and Syria
نویسندگان
چکیده
منابع مشابه
Late Cenozoic uplift along the northern Dead Sea transform in Lebanon and Syria
Evidence of long-term, late Cenozoic uplift, as well as strike-slip faulting, is revealed by topographic and geological features along the northern 500 km of the Dead Sea fault system (DSFS) – the transform boundary between the Arabian and African plates in the eastern Mediterranean region. Macro-geomorphic features are studied using a new, high-resolution (20 meter pixel) digital elevation mod...
متن کاملLate Cenozoic uplift of the Eastern Cordillera, Bolivian Andes
This paper analyses Late Cenozoic uplift in the Bolivian Andes, using the morphology of well preserved regional paleosurfaces in the Eastern Cordillera that define three axially draining braided river catchments that formed between ∼12 and ∼9 Ma. Rock uplift since the formation of the paleodrainage systems, which has been quantified using four different methods, is 1705±695 m, with a mean erosi...
متن کاملOcean Currents Modeling along the Iranian Coastline of the Oman Sea and the Northern Indian Ocean
The Makran Coast (Iranian Coastline of the Oman Sea on the Northern Indian Ocean) plays an important role in country’s future navigation and trade due to its accessibility. In 2014, the Iranian Makran coastline was selected by the PMO to be studied as the Phase 6 in the series of Monitoring and Modelling Studies of Iranian Coasts with all disciplines being in investigated including currents. Al...
متن کاملCompleting the Fertility Transition: Jordan, Lebanon and Syria
The demographic transition in the Arab countries of Western Asia in general has been somewhat peculiar. Total fertility rose substantially before it began its historical decline. Life expectancy rose at a very fast pace. The very high fertility rates, resulted in an extremely youthful populations which, combined with low mortality schedules, resulted in crude death rates (CDRs) of 3 to 4 per th...
متن کاملCrustal 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 ...
متن کاملذخیره 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: Earth and Planetary Science Letters
سال: 2006
ISSN: 0012-821X
DOI: 10.1016/j.epsl.2005.10.029