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Most zircons in marble and quartzite, typical meta-sedimentary rock from southern Sulu orogenic belt, have a core-rim structure, including an inherited detrital core and a metamorphic overgrowth rim. A few zircons are completely metamorphic. Most detrital cores have relatively high REE contents and Th/U ratios and yield highly variable 206 Pb/ 238 U ages ranging from 2828 to 211Ma,...
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