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Perthites are important disequilibrium textures found in the topaz bearing Degana Granites. Out of the two types of the perthites in the Degana Granite, the Fine-Grained stringlet type perthite is found in the unaltered portion while the dominant coarser type replacement perthite is present in the potassic alteration zones. In the present communication, a schematic model for the progressive evolution of perthite texture in the potassic alteration zone of the Degana Granite is proposed.
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