THE OCCURRENCE AND ORIGIN OF ATOLL GARNET IN HORNBLENDE SCHISTS FROM THE CONTACT AUREOLE OF THE MASHHAD GRANITE, NE IRAN

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HOMAM S.M.

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Paper Information

Journal: IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE Year:2006 | Volume:30 | Issue:A1 Page(s): 127-132

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Title

THE OCCURRENCE AND ORIGIN OF ATOLL GARNET IN HORNBLENDE SCHISTS FROM THE CONTACT AUREOLE OF THE MASHHAD GRANITE, NE IRAN

Author(s)

HOMAM S.M. | Issue Writer Certificate

Keywords

ATOLL GARNETQ3

HORNBLENDE SCHISTQ3

CONTACT AUREOLEQ3

Abstract

The formation of ATOLL GARNET in HORNBLENDE SCHISTs from the CONTACT AUREOLE of Mashhad granite, NE Iran, is discussed using textural and chemical data. These data suggest the possibility of incipient replacement of pre-existing idioblastic garnet from the core. In addition, the presence of chlorite and calcite in the core of ATOLL GARNET reveal the retrograde nature of atoll formation.

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APA: Copy

HOMAM, S.M.. (2006). THE OCCURRENCE AND ORIGIN OF ATOLL GARNET IN HORNBLENDE SCHISTS FROM THE CONTACT AUREOLE OF THE MASHHAD GRANITE, NE IRAN. IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE, 30(A1), 127-132. SID. https://sid.ir/paper/117918/en

Vancouver: Copy

HOMAM S.M.. THE OCCURRENCE AND ORIGIN OF ATOLL GARNET IN HORNBLENDE SCHISTS FROM THE CONTACT AUREOLE OF THE MASHHAD GRANITE, NE IRAN. IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE[Internet]. 2006;30(A1):127-132. Available from: https://sid.ir/paper/117918/en

IEEE: Copy

S.M. HOMAM, “THE OCCURRENCE AND ORIGIN OF ATOLL GARNET IN HORNBLENDE SCHISTS FROM THE CONTACT AUREOLE OF THE MASHHAD GRANITE, NE IRAN,” IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE, vol. 30, no. A1, pp. 127–132, 2006, [Online]. Available: https://sid.ir/paper/117918/en

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