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| | IngentaConnect Retrograde replacement of andalusite by Ca-Na mica in chloritoid-... (Site not responding. Last check: 2007-10-26) |
 | | Andalusite porphyroblasts are totally pseudomorphosed by margariteparagonite aggregates in aluminous pelites containing the peak mineral assemblage andalusite, chlorite, chloritoid, margarite, paragonite, quartz ± garnet, in a NW Iberia contact area. |
 | | Their compositions, prior to retrogression, are used in the modelling, and have been retrieved by restoring the pseudomorph-forming elements into the current-depleted matrix, except for Al which is assumed to be immobile. |
 | | Andalusite eventually disappears in relatively Al-poor rocks, resulting, as in this study, in a rock formed by chloritoidchlorite as the only FM minerals, plus margariteparagonite pseudomorphs of andalusite. |
| www.ingentaconnect.com /content/bsc/jmg/2004/00000022/00000009/art00001 (403 words) |
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