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۱SYN– TO POST–KINEMATIC FIBROLITE–BIOTITE INTERGROWTHS IN THE ARDARA AUREOLE, NW IRELAND
نویسنده(ها): ، ،
اطلاعات انتشار: Journal of Sciences، سيزدهم،شماره۴(پياپي ۵۱)، ۲۰۰۲، سال
تعداد صفحات: ۱۱
The relations of fibrolite–biotite are discussed by presenting data from the Ardara aureole, NW Ireland. Biotite–fibrolite intergrowths are developed in all three aureole zones including: the outer kyanite–bearing andalusite zone, the middle kyanite–free andalusite zone and the inner prismatic sillimanite zone. A strain–assisted mechanism is proposed for the fibrolitisation of biotite in the Ardara aureole. The concentration of fibrolite in zones of high non–coaxial strain, which wrap around zones of low co–axial strain, now occupied by minerals such as plagioclase (in the outer kyanite–bearing andalusite zone), andalusite (in the middle kyanite–free andalusite zone) and pods rich in biotite, quartz and plagioclase (in the inner sillimanite zone) provides strong evidence that fibrolite growth was syn–kinematic. Some textural evidence, especially from the inner sillimanite zone is consistent with continuation of fibrolite growth after ductile deformation.
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