Metabasic rock-hornblende schist and amphibolite occur as enclaves (50 x 30 to 90 x 60 cm size) in migmatite Horn blende and plagioclase occur as major minerals while quartz, biotite sphene and iron oxide are the minor minerals Complete re crystallization and development of schistosity have obliterated almost all the traces of parent textures and structures of the rock. The structural continuity and gradational contact between the granites and the metabasics have been discussed in the light of mineral transformation.
Cite this article:
Kuity and Lakshminarayan (1996). Mineralogical Transformations in Metabasics during Granitization around Kanker, Bastar District, M. P. Journal of Ravishankar University (Part-B: Science), 9(1), pp. 31-39.