Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Alireza Mazloumi Bajestani"'
Publikováno v:
Journal of Economic Geology, Vol 13, Iss 4, Pp 697-718 (2021)
Introduction The Neyshabour Turquoise Mine is located at 55 km North West of Neyshabour in latitude of E58◦, 23ꞌꞌ and longitude of N36◦, 23ꞌꞌ. This area is situated at the Cenozoic continental magmatic arc in the north of Sabzevar ophiol
Externí odkaz:
https://doaj.org/article/7484acec1f2e42e3afe75bd3517f3c8e
Publikováno v:
Journal of Economic Geology, Vol 12, Iss 1, Pp 111-127 (2020)
Introduction Anthropogenic activities have a high impact on urban areas and lead to severe pollution in large cities. Urban soils are huge ‘basins’ for accumulation of various pollutants. Thus, they also serve as informative media. Therefore, th
Externí odkaz:
https://doaj.org/article/354aacfd357341d79129fe20f960e0a9
Autor:
Alireza Mazloumi Bajestani, Iraj Rasa
Publikováno v:
Journal of Economic Geology, Vol 1, Iss 1, Pp 57-69 (2010)
Kuh- e -Zar gold deposit located 35 km west of Torbat-e-Heydaryeh, (Khorassan e- Razavi province), East of Iran. This deposit is a specularite-rich Iron oxide type (IOCG). This mine is situated within Khaf-Bardascan volcanic plutonic belt. Based on r
Externí odkaz:
https://doaj.org/article/874d8175a3ec4dba87c4a1e1586a0589
Autor:
Parvin Kiani, Mohammad Hakimi, Alireza Mazloumi Bajestani, Nourollah Feizi, Mina Alikhani, Paransa Alimard
Publikováno v:
Solid Fuel Chemistry. 54:337-342
In the current project, V2O5 extraction from fuel fly ash was carried out, and the advanced extraction method was investigated. This reduced the percentage of industrial fuel fly ash residue pollution in the environment. The project was done with two
Autor:
Mohammad Hassan Karimpour, Lang Farmer, Richard Keith Schader, Azadeh Malekzadeh Shafaroudi, Martiya Sadeghi, Alireza Mazloumi Bajestani, Charles R. Stern
Publikováno v:
Journal of Geochemical Exploration. 183:58-78
The Kuh-e-Zar deposit is located in the central part of the Khaf-Kashmar-Bardaskan Tertiary magmatic belt, NE Iran. The prevailing stratigraphic unit is composed of Cenozoic volcanic rocks (rhyolitic to andesitic in composition), which are intruded b