ISFAHAN

نقشه ها


گزارش ها

11. Dehagh geology surveys

Author : Ehsan Mosavi-Shahram Navavajay

Geology surveys in order to prepare the geology map

12. Feraydonshahr geology surveys

Author : Khalil Baharfiroozi- Sharam Navavajay

Geology surveys in order to prepare the geology map

13. Dehagh map geology and stratigraphy study

Author : Ehsan Mosavi -Shahram Navajay

Lab and terrestrial observations assemble

14. geophysical exploration of Shurabe sulfates in Gavkhoni

Author : Firooz Jafari

Wetland or swamp cow blood called playa Varzaneh one Playahay basin water intake in Isfahan and estuaries Zayandehrood River with an area of 550 square kilometers is. And one Frvrftgyhay Sirjan - Isfahan considered coming.

15. Radiated spectrometry in method of ICP

Author : Simin Parand

Preliminary installing of ICP system in organization by engineer Khatibi from Jam Ara Company whihcis a agent of Juben Ion Co

16. Geological science : subjects and methods

Author : gsi

Experimental science has had great development during two resent centuries and it brought many results which can be seen all of them around us and use them every day. We are used to these results as we can not feel them anymore. Look at your around, how many artificial tools can you find that are result of this sciences?

17. Radiated spectrometry in method of ICP

Author : Simin Parand

Preliminary installing of ICP system in organization by engineer Khatibi from Jam Ara Company whihcis a agent of Juben Ion Co. from France in Iran, was carried out in 1373, as monochromator, polychromator, plasma torch, spectrometer body (meta covers) and the table in front of system was installed. However complete installation of this system was in responsibility of Juben Ion engineers. This company did not accept departure of its experts to Iran till long times.

18. Regional stratigraphy of folded belt- Zagros Thrust and evolution of fore-ecosystem h is depended on it

Author : Medi Alavai

Regional stratigraphy of folded-thrust Zagros belt is revised during late neo-Proterozoic to Phanerozoic along last surveys. That includes four big lithologic groups that each groups includes several big sedimentary sequences (megasequence) which is characterized with a uncontinous border and it results from changes in sedimentary-tectonic position.


مقالات