Geochemistry data of the nadergul granodiorite of the late archean hyderabad granite batholith, part of eastern dharwar craton, india; implications for composition of the lower continental crust.

The Nadergul granodiorite (NG), is a part of Hyderabad Granite Batholith (HGB), exposed at ground level covering an area of 6 km2. Field observational data suggests that the NG is involved in the magma mixing mingling process. Petrographical data shows holocrystaline, phaneritic, coarse grained, inequigranular, mesocratic characteristics, essentially consists of quartz, orthoclase, plagioclase and microcline. The common accessory minerals are hornblende, biotite, clinopyroxene, zircon, fluorite, apatite and opaque. The myrmekitic texture is the most common intergrowth texture which seems to be magmatic origin. Geochemical data suggest that the NG is metaluminous and show calc-alkaline trend. It is charecterised by SiO2 content ranging from 63.55 % to 64.54%, moderate alkali content (Na2O + K2O = 5.6%), relatively high MgO content ranging from 2.8 % to 3.5 %. The total CaO-Na2O-K2O content ranges from 9.5 % to10.4 %. The normalised REE patterns show LREEs enrichment with slight negative europium anomaly. The High Field Strength Elements such as Zr (67.3 to 114.3 ppm), Y (21.1 to 30.1 ppm), Nb (6.3 to 8.5 ppm) and Th (8.4 to 13.8 ppm) are relatively enriched. The granodiorite is I type, falls in the Volcanic Arc Granitoid (VAG) field in tectonic discrimination diagram.

Petrology and geochemistry data of the precambrian granitoids from the Hyderabad area, part of Eastern Dharwar Craton, Telangana state India.

The data presented in this article are related to research to the research article entitled 'Petrology and Geochemistry Data of the Precambrian granitoids from the Hyderabad part of Eastern Dharwar Craton, Telangana state, India'. The granitoids from the Hyderabad area of the Telangana State are confined to the Precambrian gneissic complex of the northern-eastern part of Eastern Dharwar Craton. They cover 7760 Sq. km of the study area and fall between latitudes 16° 52'-17°42' N and between East longitudes 77° 21'-77° 51' E. The granitoids are mainly classified into grey and pink granites, granodiorites and aplites. The field studies are understood they occasionally contain older mafic enclaves in the form of lensoid bodies and thin bands and cut by younger dolerite dykes, pegmatite and quartz veins and laboratory investigations resolved the classification of the granitods and their chemical histories.