Sendra Granite Sendra Granite Sendra Granite is a plutonic igneous rock population which is part of Delhi supergroup of meta-sedimentary rocks located along NH-8 in Rajasthan, India. It has undergone years of sculpting by wind and air. It was declared as a Geoheritage Site by the Geological Survey of India in 1977. It is located at a Latitude of -26° 05´ 3.6" N and a Longitude of -74° 13´ 17.8" E and is at a height of 429.6 ± 5.7 m above sea level. Sendra Granite is located in the Pali district of Rajasthan in the north-west of India. The Sendra Granite
A-type granite magnesium. There are lower levels of calcium and strontium. By using Ga/Al ratio, fractionated felsic I or S-type granites can overlap in apparent composition. Enriched alkalis include sodium, potassium, rubidium and caesium. Other depleted elements include barium, phosphorus, titanium and europium. Subtypes include A, anorogenic, derived from ocean island basalt; and A post-orogenic, derived by crustal melting or crust and mantle mixing. The source could be dry granulite left over from the loss of wet magma during orogenies. A-type granite A-type granites are a class of granite. They are characterised by low water and a lack of tectonic fabric. A