ORIGIN OF GARNET ZONING IN THE CONTACT METAMORPHIC AREOLE OF HASSAN-ABAAD INTRUSION, SOUTHWEST OF TAFT

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.

ZANDIFAR S.; VALIZADEH M.V.; BARGHI M.A.

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

Journal Paper

Paper Information

Journal: JOURNAL OF ECONOMIC GEOLOGY Year:2010 | Volume:1 | Issue:1 Page(s): 71-82

Download Full-Text

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

Persian Verion

View:

1,376

Download:

Cites:

Information Journal Paper

Title

ORIGIN OF GARNET ZONING IN THE CONTACT METAMORPHIC AREOLE OF HASSAN-ABAAD INTRUSION, SOUTHWEST OF TAFT

Author(s)

ZANDIFAR S. | VALIZADEH M.V. | BARGHI M.A. | Issue Writer Certificate

Keywords

GARNETQ2

ZONINGQ2

CONTACT METAMORPHICQ2

HASSAN-ABAAD VILLAGEQ3

YAZDQ2

Abstract

In the CONTACT METAMORPHIC aureole of the next to the granodiorite intrusive body in the HASSAN-ABAAD VILLAGE of YAZD, high frequency GARNET in different metamorphic zones is notable, which some contain GARNET crystal with obvious ZONING. Obtained data from core to rim of GARNET by SEM point analysis, show that GARNET crystals belong to grandite series, and sharp variation of Al and Fe from center to rim indicates GARNET ZONING formed during crystal growth, but the ZONING has been disturbed by fluid infiltration next to fractures. Researching on mineral variations from core to rim indicates that the main factor on the formation of oscillatory ZONING was immiscibility in grandite series and followed by changes in hydrothermal solution composition.

Cites

No record.

References

No record.

Cite

APA: Copy

ZANDIFAR, S., VALIZADEH, M.V., & BARGHI, M.A.. (2010). ORIGIN OF GARNET ZONING IN THE CONTACT METAMORPHIC AREOLE OF HASSAN-ABAAD INTRUSION, SOUTHWEST OF TAFT. JOURNAL OF ECONOMIC GEOLOGY, 1(1), 71-82. SID. https://sid.ir/paper/180548/en

Vancouver: Copy

ZANDIFAR S., VALIZADEH M.V., BARGHI M.A.. ORIGIN OF GARNET ZONING IN THE CONTACT METAMORPHIC AREOLE OF HASSAN-ABAAD INTRUSION, SOUTHWEST OF TAFT. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2010;1(1):71-82. Available from: https://sid.ir/paper/180548/en

IEEE: Copy

S. ZANDIFAR, M.V. VALIZADEH, and M.A. BARGHI, “ORIGIN OF GARNET ZONING IN THE CONTACT METAMORPHIC AREOLE OF HASSAN-ABAAD INTRUSION, SOUTHWEST OF TAFT,” JOURNAL OF ECONOMIC GEOLOGY, vol. 1, no. 1, pp. 71–82, 2010, [Online]. Available: https://sid.ir/paper/180548/en

Related Journal Papers