Development of Perthite in the Topaz Bearing Degana Granite, Rajasthan

Authors

  • Department of Geology, University of Jammu, Jammu - 180 006
  • Department of Geology, University of Jammu, Jammu - 180 006

Abstract

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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Short Communications

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Published

2005-06-01

How to Cite

Sukhchain, ., & Srivastava, P. K. (2005). Development of Perthite in the Topaz Bearing Degana Granite, Rajasthan. Journal of Geological Society of India, 65(6), 758–761. Retrieved from https://www.geosocindia.com/index.php/jgsi/article/view/82452