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The Sandmata Complex in Rajasthan within the NW Indian shield represents a metamorphosed volcano-sedimentary sequence incorporated within a late Paleoproterozoic suture zone. Here we report laser ablation ICP-MS age data and REE geochemistry of zircons from four rock types in the Sandmata Complex – a foliated biotite–quartz gneiss, a leucocratic gneiss, a biotite gneiss and a porphyritic granite....
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