نتایج جستجو برای: upper red formation

تعداد نتایج: 861952  

Journal: :desert 2013
a. kouhpeima s. feiznia h. ahmadi s.a. asghar hashemi h. ghadimi

this contribution determines suitable fingerprinting properties for sediment source discrimination within theamrovan and atary catchments in semnan province, iran. these catchments are representative of a range of geology formations and should therefore provide a meaningful basis for a general assessment of the degree of sediment source discrimination afforded by a range of fingerprint properti...

Two stratigraphic sections (Kuh-e-Rahmat and Kuh-e-Sabz) of Upper Cretaceous strata in the Interior Fars region (SW of Iran) were selected. Lower Cretaceous succession of Kuh-e-Rahmat was consisted of Dariyan, Kazhdumi Sarvak and Ilam Formations. The lower contact of the Sarvak Formation with Kazhdumi Formation is described as a transitional type whereas the upper contact of Sarvak Formation wa...

Journal: :journal of agricultural science and technology 2011
a. kouhpeima s. feiznia h. ahmadi s. a. a. hashemi

sediment yield data, collected for most regions in iran has been insufficient and not so reliable and there is still not any sufficiently reliable methodology available for sediment yield assessment in the country as a whole. on the other hand, an attainment of reliable sediment yield data is a must and key requirement for the design of effective sediment management as well as control strategie...

Journal: :journal of sciences islamic republic of iran 0

lithological characteristics of the asmari formation in the burujen area are: pelagic foraminifera wackestone-packstone; bentic foraminifera echinid packstone; bentic foraminifera corallinaceapackstone; coral boundstone and echinid corallinacea packstone to grainstone; corallinacea boundstone; corallinacea bryozoa packstone; rniliolid echinid wackestone; and bioclastic wackestone. the examined ...

Journal: :Journal of experimental botany 2005
Koldobika Hormaetxe José María Becerril Isabel Fleck Marta Pintó José Ignacio García-Plazaola

Red (retro)-carotenoids accumulate in chloroplasts of Buxus sempervirens leaves during the process of winter leaf acclimation. As a result of their irregular presence, different leaf colour phenotypes can be found simultaneously in the same location. Five different colour phenotypes (green, brown, red, orange, and yellow), with a distinct pattern of pigment distribution and concentration, have ...

ژورنال: مواد پرانرژی 2015
فتاحی, حسن , اسماعیل زاده, رحیمه , فرازمند, رامین , موسائی اسکوئی, یونس,

In order to use TNT in military industries, its impurities have to be removed. The further nitration of m-nitrotoluene (by-product of the first step nitration), cause to the formation of asymmetric products which during the purification step, these tri-nitrated and asymmetric products lead to the formation of red water as a main environmental pollutant. This pollutant remains in the environment...

Journal: :The Journal of the Geological Society of Japan 1958

Journal: :فیزیک زمین و فضا 0
محمد مرادی امیرحسین مشکواتی مجید آزادی عباسعلی علی اکبری بیدختی

orography plays a substantial role in the formation and evolution of many atmospheric phenomena. observations indicate that two mountain ranges to the southwest of the red sea and west of iran (zagross mountain range) play a crucial role in the formation, evolution and activities of synoptic weather systems over iran. observations also, indicate that there are considerable differences between t...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2004
Neil D Opdyke Victor J DiVenere

Three sections of Chesterian Mauch Chunk Formation in Pennsylvania have been studied paleomagnetically to determine a Late Mississippian magnetic polarity stratigraphy. The upper section at Lavelle includes a conglomerate with abundant red siltstone rip-up clasts that yielded a positive conglomerate test. All samples were subjected to progressive thermal demagnetization to temperatures as high ...

Lithological characteristics of the Asmari Formation in the Burujen area are: pelagic foraminifera wackestone-packstone; bentic foraminifera echinid packstone; bentic foraminifera corallinaceapackstone; coral boundstone and echinid corallinacea packstone to grainstone; corallinacea boundstone; corallinacea bryozoa packstone; rniliolid echinid wackestone; and bioclastic wackestone. The exami...

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