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The granitoids of the study area, especially the gneissic granitoids, comprise felsic and mafic lenticular enclaves of different sizes. Petrographically older and younger granitoids show medium to fine-grained, porphyritic and inequigranular textures. The gneissic rocks show foliation. At the contact of mafic enclaves and gneissic zones, conspicuous variation in mineralogy is observed in thin-sections. Presence of enclaves indicates coexistence and mixing of both felsic and mafic magmas at the source. The typical textures like perthitic, graphics and lamellar twinning indicate a direct magmatic origin for these granitoid rocks. The presence of pyrite mineralization at Khatgaon indicates late stage hydrothermal activity associated with felsic veins.
By P. R.C.Phani | N. Ningam | M. Srinivas" Field Geology and Petrography of Granitoid rocks in southeastern part of Nanded district, Maharashtra State"
Published in International Journal of Trend in Scientific Research and Development (ijtsrd), ISSN: 2456-6470, Volume-1 | Issue-6 , October 2017,
Paper URL: http://www.ijtsrd.com/papers/ijtsrd4710.pdf
Direct URL: http://www.ijtsrd.com/other-scientific-research-area/geology/4710/field-geology-and-petrography-of-granitoid-rocks-in-southeastern-part-of-nanded-district-maharashtra-state/p-rcphani
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