Characteristics of mineralogy, geochemistry and genesis conditions of Damghan fluorite deposit

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

riahimah m.; HASSANNEZHAD A.A.; Vahabzadeh kebriya g.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: Researches in Earth Sciences Year:2015 | Volume:6 | Issue:22 Page(s): 51-64

Download Full-Text

Persian Verion

View:

562

Download:

Cites:

Information Journal Paper

Title

Characteristics of mineralogy, geochemistry and genesis conditions of Damghan fluorite deposit

Author(s)

riahimah m. | HASSANNEZHAD A.A. | Vahabzadeh kebriya g. | Issue Writer Certificate

Keywords

DamghanQ2

FluoriteQ1

Fluid inclusionsQ1

GeochemistryQ2

Abstract

Damghan Fluorite deposit (south of Aresk) is located in the north-west of Damghan. This deposit is limited to the Arsk Mountains and from south it limited to the Atary fault. The mineralized zone is located in member 1 of the mila formation which is mostly dolomite along with interbeds of marl and yellow shal (yellow shal has the same age as middle Cambrian). Fluorite mineralization is mostly white color and a lesser amount with violate color and it is occurred as vein or open space filling. Along with Fluorite mineralization, other minerals could be seen as sulfide minerals (like galena, pyrite, chalcopyrite, coveline) and also cerussite minerals, iron hydroxides, calcite and barite. According to the micro thermometry data carried out on Fluid inclusions of white and violate Fluorite, the temperature domain of homogenization is changing between 100 to 360 ° C and the salinity domain of mineralizing fluid is changing between 0. 2 to 20. 2 wt% NaCl equ. . Evidence shows that Fluorite mineralization probably occurred from mixing of hydrothermal fluid with meteoric and basinal fluids in reducing conditions.

Multimedia

No record.

Cites

No record.

References

No record.

Cite

APA: Copy

riahimah, m., HASSANNEZHAD, A.A., & Vahabzadeh kebriya, g.. (2015). Characteristics of mineralogy, geochemistry and genesis conditions of Damghan fluorite deposit. RESEARCHES IN EARTH SCIENCES, 6(22 ), 51-64. SID. https://sid.ir/paper/207451/en

Vancouver: Copy

riahimah m., HASSANNEZHAD A.A., Vahabzadeh kebriya g.. Characteristics of mineralogy, geochemistry and genesis conditions of Damghan fluorite deposit. RESEARCHES IN EARTH SCIENCES[Internet]. 2015;6(22 ):51-64. Available from: https://sid.ir/paper/207451/en

IEEE: Copy

m. riahimah, A.A. HASSANNEZHAD, and g. Vahabzadeh kebriya, “Characteristics of mineralogy, geochemistry and genesis conditions of Damghan fluorite deposit,” RESEARCHES IN EARTH SCIENCES, vol. 6, no. 22 , pp. 51–64, 2015, [Online]. Available: https://sid.ir/paper/207451/en

Related Journal Papers