Dolomitization model and its relation to mineralization in Hasan Abad Lead, Zinc and Barite deposit (Northeast of Esfahan)

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.

AHMADI SANAZ; SALEHI MOHAMMADALI; JAMALI H.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2020 | Volume:29 | Issue:116 Page(s): 23-34

Download Full-Text

Persian Verion

View:

397

Download:

Cites:

Information Journal Paper

Title

Dolomitization model and its relation to mineralization in Hasan Abad Lead, Zinc and Barite deposit (Northeast of Esfahan)

Author(s)

AHMADI SANAZ | SALEHI MOHAMMADALI | JAMALI H. | Issue Writer Certificate

Keywords

LeadQ2

zincQ2

PetrographyQ2

GeochemistryQ1

The dolomitization modelQ1

Hasan AbadQ1

Abstract

The Hassan Abad Zn-Pb deposits is located in the northeast of Isfahan, Central Iran zone. The host rock of this mineralization is the dolomite of Middle Triassic Shotori Formation. Mineralization included galena, sphalerite, sulfosalts, pyrite and barite which associated with dolomitization. Based on petrographic studies six types of dolomites (in terms of shape and size of the crystals, the distribution of crystal size and shape of the border crystal) has been identified, that including very fine, medium, coarsely crystalline dolomite, Saddle dolomites and filling pore spaces and veins. The first and second type of dolomites were formed as synsedimentary or diagenetic dolomite with sabkha origin. The third type of dolomite in the late stages of diagenesis was formed in shallow burial conditions due to recrystallization of small crystalline dolomite. Coarse-grained and saddle dolomites have been created under the conditions of deep burial and as hydrothermal dolomites and are related to mineralization. Move over, the origin of magnesium for fine crystalline dolomites were seawater, and for coarse crystalline dolomites are probably the brine fluids of the compacted Sorkh Shale Formation and hydrothermal fluid.

Cites

No record.

References

No record.

Cite

APA: Copy

AHMADI, SANAZ, SALEHI, MOHAMMADALI, & JAMALI, H.. (2020). Dolomitization model and its relation to mineralization in Hasan Abad Lead, Zinc and Barite deposit (Northeast of Esfahan). GEOSCIENCES, 29(116 ), 23-34. SID. https://sid.ir/paper/392183/en

Vancouver: Copy

AHMADI SANAZ, SALEHI MOHAMMADALI, JAMALI H.. Dolomitization model and its relation to mineralization in Hasan Abad Lead, Zinc and Barite deposit (Northeast of Esfahan). GEOSCIENCES[Internet]. 2020;29(116 ):23-34. Available from: https://sid.ir/paper/392183/en

IEEE: Copy

SANAZ AHMADI, MOHAMMADALI SALEHI, and H. JAMALI, “Dolomitization model and its relation to mineralization in Hasan Abad Lead, Zinc and Barite deposit (Northeast of Esfahan),” GEOSCIENCES, vol. 29, no. 116 , pp. 23–34, 2020, [Online]. Available: https://sid.ir/paper/392183/en

Related Journal Papers