منابع مشابه
Late Miocene River Euphrates
1 Department of Geography, Harran University, 63300 Şanlıurfa, Turkey 2 Isotope Geosciences Laboratory, Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139-4307, USA 3 Department of Geology, Çukurova University, 01330 Adana, Turkey 4 Faculty of Mathematics and Computing, The Open University, Eldon House, Gosforth, Newcastle-upon-T...
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karyotype of river loach turcinoemacheilus kosswigi from the euphrates river, turkey was investigated using conventional giemsa-staining and c-banding. two females and two males were analyzed. diploid chromosome number was 2n= 50 in all specimens. the karyotype consisted of four pairs of metacentric (m), seven pairs of submeta (sm)-subtelocentric (st) and 14 pairs of acrocentric (a) chromosomes...
متن کاملLocation of the River Euphrates in the Late Miocene; dating of terrace gravel at Shireen, Syria
We report gravel of the River Euphrates, capped by basalt that is Ar-Ar dated to ∼9 Ma, at Shireen in northern Syria. This gravel, preserved by the erosion-resistant basalt, allows us for the first time to reconstruct the history of this major river during the Late Miocene. In response to progressive regional surface uplift, the Euphrates extended SE by ∼800 km between the early Middle Miocene,...
متن کاملMajor, Trace and REE geochemistry of Paleo-Tethys Collision-Related Granitoids from Mashhad, Iran
متن کامل
Mineralogy and geochemistry of major, trace and REE elements, Pirashkaft Bauxite Deposits, Mamasani, Fars Province
The Pirashkaft bauxite deposit is located in north of the Paskuhak anticline in the Fars Province. The bauxite deposit present between Sarvak and Gurpy Formations, and formed during the Late Turonian time as a consequent of the Laramid orogeny phase. According to the geological investigations, the Pirashkaft bauxite is Karstic type. The residual ore studied in the Pirashkaft can be classified ...
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ژورنال
عنوان ژورنال: Journal of Chemistry
سال: 2016
ISSN: 2090-9063,2090-9071
DOI: 10.1155/2016/1012021