THE MECHANISM OF FIBROLITE FORMATION IN THE CONTACT AUREOLE OF MASHHAD GRANITE

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HOMAM S.M.; GHAEMI FAROKH

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Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2008 | Volume:16 | Issue:1 Page(s): 159-168

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Title

THE MECHANISM OF FIBROLITE FORMATION IN THE CONTACT AUREOLE OF MASHHAD GRANITE

Author(s)

HOMAM S.M. | GHAEMI FAROKH | Issue Writer Certificate

Keywords

FIBROLITEQ3

CONTACT AUREOLEQ3

MASHHAD METAMORPHIC ZONEQ3

METASOMATISMQ2

CATION LEACHINGQ3

Abstract

The mechanism of FIBROLITE formation in metapelitic rocks of the CONTACT AUREOLE of Mashhad granite is examined in this study. According to textural features, FIBROLITE considered to be disharmonious. Textural evidence strongly suggests that most of the FIBROLITE in this aureole are formed by decomposition of biotite. FIBROLITE produced late in the thermal history of the aureole through a reaction involving acidic volatiles emanating from the adjacent intrusion. Textural evidence suggests that the FIBROLITE formed at temperatures within the andalusite stability field in the aureole investigated in this study.

Cites

References

FIBROLITE FORMATION IN THE CHAHGHAND GABBRODIORITE CONTACT AUREOLE, NE NEYRIZ, SOUTHERN IRAN

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APA: Copy

HOMAM, S.M., & GHAEMI, FAROKH. (2008). THE MECHANISM OF FIBROLITE FORMATION IN THE CONTACT AUREOLE OF MASHHAD GRANITE. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 16(1), 159-168. SID. https://sid.ir/paper/3865/en

Vancouver: Copy

HOMAM S.M., GHAEMI FAROKH. THE MECHANISM OF FIBROLITE FORMATION IN THE CONTACT AUREOLE OF MASHHAD GRANITE. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2008;16(1):159-168. Available from: https://sid.ir/paper/3865/en

IEEE: Copy

S.M. HOMAM, and FAROKH GHAEMI, “THE MECHANISM OF FIBROLITE FORMATION IN THE CONTACT AUREOLE OF MASHHAD GRANITE,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 16, no. 1, pp. 159–168, 2008, [Online]. Available: https://sid.ir/paper/3865/en

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