MINERALOGY, GEOCHEMISTRY AND GENESIS OF CARBONATE– SILICA SERPENTINES (LISTWAENITE) IN NORTH OF NAIN OPHIOLITE (WEST OF CENTRAL IRAN)

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.

SAIDI M.; FALAHATI S.; NOGHREYAN M.; KHALILI M.; GHAHRAIPOUR M.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2009 | Volume:17 | Issue:3 Page(s): 405-418

Download Full-Text

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

Persian Verion

View:

1,144

Download:

Cites:

Information Journal Paper

Title

MINERALOGY, GEOCHEMISTRY AND GENESIS OF CARBONATE– SILICA SERPENTINES (LISTWAENITE) IN NORTH OF NAIN OPHIOLITE (WEST OF CENTRAL IRAN)

Author(s)

Keywords

PERIDOTITESQ2

LISTWAENITEQ3

NAIN OPHIOLITEQ2

MERCURYQ3

Abstract

The mantle sequence serpentinized PERIDOTITES of north of Nain have been converted to carbonate- silica assemblage known as LISTWAENITE at various temperature and pH in response to CO2 and SiO2 bearing fluids. On the basis of carbonate and silica minerals content, three types of LISTWAENITE have been recognized: carbonate, carbonate- silica and silica LISTWAENITEs. Generaly carbonate minerals are magnesite, dolomite, ferrite-dolomite and ankerite. Calcite and other carbonate minerals are rare. Silica minerals (including quartz, chalcedony and chert) accompanied by accessory Cr-spinel, chlorite, sulfide minerals also occur in LISTWAENITEs. Silica matrix in silica LISTWAENITE containing high amounts of Hg, Ag and As elements and shows that these elements have transported by SiO2 bearing hydrothermal fluids as arsenide complexes.

Cites

No record.

References

MINERALOGY, GEOCHEMISTRY, STRUCTURAL POSITION AND A GENETIC MODEL FOR LISTVENITE IN EAST OF IRAN

Cite

APA: Copy

SAIDI, M., FALAHATI, S., NOGHREYAN, M., KHALILI, M., & GHAHRAIPOUR, M.. (2009). MINERALOGY, GEOCHEMISTRY AND GENESIS OF CARBONATE– SILICA SERPENTINES (LISTWAENITE) IN NORTH OF NAIN OPHIOLITE (WEST OF CENTRAL IRAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 17(3), 405-418. SID. https://sid.ir/paper/4187/en

Vancouver: Copy

SAIDI M., FALAHATI S., NOGHREYAN M., KHALILI M., GHAHRAIPOUR M.. MINERALOGY, GEOCHEMISTRY AND GENESIS OF CARBONATE– SILICA SERPENTINES (LISTWAENITE) IN NORTH OF NAIN OPHIOLITE (WEST OF CENTRAL IRAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2009;17(3):405-418. Available from: https://sid.ir/paper/4187/en

IEEE: Copy

M. SAIDI, S. FALAHATI, M. NOGHREYAN, M. KHALILI, and M. GHAHRAIPOUR, “MINERALOGY, GEOCHEMISTRY AND GENESIS OF CARBONATE– SILICA SERPENTINES (LISTWAENITE) IN NORTH OF NAIN OPHIOLITE (WEST OF CENTRAL IRAN),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 17, no. 3, pp. 405–418, 2009, [Online]. Available: https://sid.ir/paper/4187/en

Related Journal Papers