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Peninsular Gneiss information


Peninsular Gneiss or Peninsular Gniessic Complex are the gneissic complex of the metamorphics found all over the Indian Peninsula, on top of which, the supra-crustal Dharwar System have been laid down.[1] The term was first fashioned by W.F.Smeeth of the Mysore Geological Department in 1916 based on the first scientific study of this rock exposure. One of the best exposures of this rock mass, dated 2.5 to 3.4 billion years, is located at Lal Bagh in Bangalore.[2][3] The exposure is also called the Lalbagh rock.[4]

  1. ^ Naha, K.; Srinivasan, R.; Jayaram, S. (1 February 1990). "Structural evolution of the Peninsular Gneiss — an early Precambrian migmatitic complex from South India". Geologische Rundschau. 79 (1): 99–109. doi:10.1007/BF01830449. ISSN 1432-1149.
  2. ^ "Peninsular Gneiss". Geological Survey of India. Archived from the original on 21 July 2011. Retrieved 27 February 2009.
  3. ^ National Geological Monuments, pages 96, Peninsular Gneiss,page29-32. Geological Survey of India,27, Jawaharlal Nehru Road, Kolkata-700016. 2001. ISSN 0254-0436.
  4. ^ "Lalbagh - Abounting with natural landmarks". Tourism Karnataka. Archived from the original on 5 January 2009. Retrieved 28 February 2009.

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