KYANITE IN THERMAL AUREOLES

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HOMAM S.M.; ATHERTON M.P.; BOYLE A.P.

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Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2004 | Volume:12 | Issue:1 Page(s): 105-128

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Information Journal Paper

Title

KYANITE IN THERMAL AUREOLES

Author(s)

HOMAM S.M. | ATHERTON M.P. | BOYLE A.P. | Issue Writer Certificate

Keywords

KYANITEQ2

ALUMINIUM SILICATESQ4

CONTACT AUREOLEQ3

Abstract

Different models are discussed to interpret the presence of KYANITE as a stable phase in CONTACT AUREOLEs especially in the andalusite-, sillimanite- bearing aureoles. In such aureoles the polymorphic sequence KYANITE → andalusite → sillimanite can be explained in tenns of an essentially isobaric path during which KYANITE initially crystallises from the breakdown of pyrophyllite or more likely muscovite + chlorite beneath the pressure of the triple point (3-4 kbar 10-14 km depth), followed by andalusite and sillimanite crystallisation. The sequence KYANITE-sillimanite and/or fibrolite can be seen in thennal aureoles subjected to isobaric metamorphism above the triple Al2SiO5 point (5-8 kbar 17-28 km depth). The absence of KYANITE in some thennal aureoles can be explained on the basis of either compositional constraint or overstepping of low- temperature reactions due to high heating rates.

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APA: Copy

HOMAM, S.M., ATHERTON, M.P., & BOYLE, A.P.. (2004). KYANITE IN THERMAL AUREOLES. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 12(1), 105-128. SID. https://sid.ir/paper/3805/en

Vancouver: Copy

HOMAM S.M., ATHERTON M.P., BOYLE A.P.. KYANITE IN THERMAL AUREOLES. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2004;12(1):105-128. Available from: https://sid.ir/paper/3805/en

IEEE: Copy

S.M. HOMAM, M.P. ATHERTON, and A.P. BOYLE, “KYANITE IN THERMAL AUREOLES,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 12, no. 1, pp. 105–128, 2004, [Online]. Available: https://sid.ir/paper/3805/en

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