Records of the Geological Survey of India, Volume 115, Parts 3-6The Survey, 1986 - Earthquakes Vols. 1- include Report of the Geological Survey, 1867- ; v. 32- include Review of the mineral production of India, 1898/1903- ; v. 75 consists of Professional papers, no. 1-16; v. 76 consists of Bulletins of economic minerals. |
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Page 54
... heat only by conduction . The area seems to have higher heat flow which is heating water . However , isotope sampling of the area around Tattapani would have to be done to ascertain the migration channels of water . Age dating of ...
... heat only by conduction . The area seems to have higher heat flow which is heating water . However , isotope sampling of the area around Tattapani would have to be done to ascertain the migration channels of water . Age dating of ...
Page 95
... heat by radioactive decay the heating by normal temperature gradient is sugges- ted . The water with ambient temperature of 20oC would have to percolate to about 660 m to attain a temperature of 40 ° C . ACKNOWLDGEMENTS Authors are ...
... heat by radioactive decay the heating by normal temperature gradient is sugges- ted . The water with ambient temperature of 20oC would have to percolate to about 660 m to attain a temperature of 40 ° C . ACKNOWLDGEMENTS Authors are ...
Page 134
... heat loss from Unhavre ( Khed ) hot spring itself is to be of the order of 2944 KW ( Thermal ) and possibility of contineous recharges of the reservoir at depth can be much larger . Minimum heat energy available at other hot spring is ...
... heat loss from Unhavre ( Khed ) hot spring itself is to be of the order of 2944 KW ( Thermal ) and possibility of contineous recharges of the reservoir at depth can be much larger . Minimum heat energy available at other hot spring is ...
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Common terms and phrases
alkaline alluvium Anhoni anomaly Barail basalt basin belt biotite bore hole borehole carbonatite channel charnockite chloride cyclone Deccan Trap deposits depth discharge district drilling dykes Formation fracture garnet Geol Geological Survey geophysical geothermal system gneiss Gondwana gradient grains granulite grey GSI Rec 115 hills hornblende hot spring hot spring area hot water indicate Khed kimberlite lamprophyres laterite limestone lineament located Madhya Pradesh magnetite Maharashtra Meghalaya metres mineral mineralisation Muthuraman Nala ND ND ND occur olivine pipe rocks Proterozoic pyroxene quartz range Rec 115 pts region reservoir river Salbardi samples sand sandstone Sativli schist sediments shale soil structural studies stylolites surface Surguja Surv Survey of India taluk Tattapani fault TATTAPANI HOT SPRING temperature thermal manifestation thermal springs thermal waters thickness Thussu trap flow trending Trichinopoly Tural Unhavre Khed Unpub upflow zone upto Uttattur Vajrakarur valley values width