Geology, geochemistry and genesis of the iron mineralization in Jurassic volcano-sedimentary sequence of the Dash Aghol deposit, Northeast of Bukan, Sanandaj-Sirjan zone

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.

MAGHFOURI S.; MOVAHEDNIA M.; HOSSEINZADEH M.R.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Geology Year:2019 | Volume:13 | Issue:50 Page(s): 75-88

Download Full-Text

View:

215

Download:

Cites:

Information Journal Paper

Title

Geology, geochemistry and genesis of the iron mineralization in Jurassic volcano-sedimentary sequence of the Dash Aghol deposit, Northeast of Bukan, Sanandaj-Sirjan zone

Author(s)

MAGHFOURI S. | MOVAHEDNIA M. | HOSSEINZADEH M.R. | Issue Writer Certificate

Keywords

Stratiform

Sandstone-Limey tuff

Jurassic

Dash Aghol iron ore

Bukan

Abstract

The Dash Aghol iron deposit is located in the northeast of Bukan city and is hosted by Jurassic volcano-sedimentary sequence. The main host rock of the Dash Aghol deposit includes sandstone, limy tuff and limestone. Based on geometry of ore body, two different types of mineralization were distinguished in Dash Aghol deposit: lenticular primary mineralization which occurred as parallel and concordant with layering of the host rocks. Ore textures of this type include massive, laminated and disseminated forms existing in sandstone, limy tuff and limestone. Second type, includes supergene vein-veinlet and open space filling mineralization which is associated with faults and related brecciated zones and were occurred in hanging wall rocks of the primary ore lense. According to the stratigraphy, ore body form, texture, paragenetic sequences, ore bearing chert-carbonate-tuff facies and mineralogy, the iron mieralization in Dash Aghol deposit is Stratiform tuff carbonate-sandstone host rocks deposits, in rolcano-sedimentary sequence of Jurassic, which were precipitated in shallow marine environment.

Cites

No record.

References

No record.

Cite

APA: Copy

MAGHFOURI, S., MOVAHEDNIA, M., & HOSSEINZADEH, M.R.. (2019). Geology, geochemistry and genesis of the iron mineralization in Jurassic volcano-sedimentary sequence of the Dash Aghol deposit, Northeast of Bukan, Sanandaj-Sirjan zone. IRANIAN JOURNAL OF GEOLOGY, 13(50 ), 75-88. SID. https://sid.ir/paper/726697/en

Vancouver: Copy

MAGHFOURI S., MOVAHEDNIA M., HOSSEINZADEH M.R.. Geology, geochemistry and genesis of the iron mineralization in Jurassic volcano-sedimentary sequence of the Dash Aghol deposit, Northeast of Bukan, Sanandaj-Sirjan zone. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2019;13(50 ):75-88. Available from: https://sid.ir/paper/726697/en

IEEE: Copy

S. MAGHFOURI, M. MOVAHEDNIA, and M.R. HOSSEINZADEH, “Geology, geochemistry and genesis of the iron mineralization in Jurassic volcano-sedimentary sequence of the Dash Aghol deposit, Northeast of Bukan, Sanandaj-Sirjan zone,” IRANIAN JOURNAL OF GEOLOGY, vol. 13, no. 50 , pp. 75–88, 2019, [Online]. Available: https://sid.ir/paper/726697/en

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans

No record.

Recommended Workshops