ORIGIN OF SCAPOLITE IN PLUTONIC ROCKS OF PANJ - KUH (SOUTH-EAST OF DAMGHAN)

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.

ESMAEILI DARYOUSH; SHIBI M.; KANANIAN A.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2004 | Volume:12 | Issue:2 Page(s): 189-201

Download Full-Text

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

Persian Verion

View:

872

Download:

Cites:

Information Journal Paper

Title

ORIGIN OF SCAPOLITE IN PLUTONIC ROCKS OF PANJ - KUH (SOUTH-EAST OF DAMGHAN)

Author(s)

ESMAEILI DARYOUSH | SHIBI M. | KANANIAN A. | Issue Writer Certificate

Keywords

MINERALOGYQ4

SCAPOLITEQ4

PANJ - KUHQ4

DAMGHANQ4

ALKALI METASOMATISMQ2

Abstract

The MINERALOGY and origin of the SCAPOLITE crystals of the Panj-Kuh area (S-E DAMGHAN) has been investigated. Based on textural and field observations, two types of SCAPOLITE have been identified. Type 1 SCAPOLITE consists of fine to coarse grain crystals which are mainly replaced for plagioclase in the pluton body. The type 2 as veinlet and vein ranging in thickness from few milimeters inside the body to about few hundred meters in the margin of the body that present close to the iron ore deposit. It seems that the formation of the first type of SCAPOLITEs is related to the circulation of NaCl rich fluid around of the intrusive body, and the second type has directly been precipitated from the hydrothermal fluids. The extensive abundance of SCAPOLITE-albite zone in intrusive rocks and specially between body and a volcano-sedimentary sequence suggest that the formation of SCAPOLITE was accompanied by an ALKALI METASOMATISM which has been derived from the evaporate sediments of that sequences.

Cites

PETROGENESIS AND EVOLUTION OF PANJ-KUH IRON SKARN (EASTERN IRAN)

References

No record.

Cite

APA: Copy

ESMAEILI, DARYOUSH, SHIBI, M., & KANANIAN, A.. (2004). ORIGIN OF SCAPOLITE IN PLUTONIC ROCKS OF PANJ - KUH (SOUTH-EAST OF DAMGHAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 12(2), 189-201. SID. https://sid.ir/paper/3877/en

Vancouver: Copy

ESMAEILI DARYOUSH, SHIBI M., KANANIAN A.. ORIGIN OF SCAPOLITE IN PLUTONIC ROCKS OF PANJ - KUH (SOUTH-EAST OF DAMGHAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2004;12(2):189-201. Available from: https://sid.ir/paper/3877/en

IEEE: Copy

DARYOUSH ESMAEILI, M. SHIBI, and A. KANANIAN, “ORIGIN OF SCAPOLITE IN PLUTONIC ROCKS OF PANJ - KUH (SOUTH-EAST OF DAMGHAN),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 12, no. 2, pp. 189–201, 2004, [Online]. Available: https://sid.ir/paper/3877/en

Related Journal Papers