Records of the Geological Survey of IndiaGeological Survey of India, 1939 - 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 iv
... shows one of the felspathic patches in Fig . 1 under crossed nicols . The granulation and disconti nuity of the twinning planes is due to crushing and move- ment . FIG . 3. - Charnockite similar to that shown in Fig . 1 , but more ...
... shows one of the felspathic patches in Fig . 1 under crossed nicols . The granulation and disconti nuity of the twinning planes is due to crushing and move- ment . FIG . 3. - Charnockite similar to that shown in Fig . 1 , but more ...
Page 14
... show - cases in the museum was continued , as also the rearrangement of stored rock and duplicate collections . Thorough overhauling of the meteorite collections was ably undertaken by Dr. Coulson during the year , 19. Presentations of ...
... show - cases in the museum was continued , as also the rearrangement of stored rock and duplicate collections . Thorough overhauling of the meteorite collections was ably undertaken by Dr. Coulson during the year , 19. Presentations of ...
Page 29
... shows : - Sio , A1,03 Fe , 0 , Tio , CaO MgO Alkalies • 1.27 58.64 · 3.16 · 12.12 · 0.16 • 0.18 0.12 · 24.12 Loss on ignition 99.77 The other area lies immediately to the south - west of Daunapat ( 23 ° 1 ′ : 84 ° 5 ′ ) , at an ...
... shows : - Sio , A1,03 Fe , 0 , Tio , CaO MgO Alkalies • 1.27 58.64 · 3.16 · 12.12 · 0.16 • 0.18 0.12 · 24.12 Loss on ignition 99.77 The other area lies immediately to the south - west of Daunapat ( 23 ° 1 ′ : 84 ° 5 ′ ) , at an ...
Page 38
... shows that dirt and debris must have accumulated to a height of about 4 to 4 ft . from the floor , the walls to that height showing deep decay due to the action of accumulated salts . In 1935 , some fragments of the sculptured figures ...
... shows that dirt and debris must have accumulated to a height of about 4 to 4 ft . from the floor , the walls to that height showing deep decay due to the action of accumulated salts . In 1935 , some fragments of the sculptured figures ...
Page 51
... shows that the under - ground water- table at Jashpurnagar is about 30-45 ft . below the surface . At these depths the wells appear to have low recuperative powers . If , therefore , the site for the new well be selected in the doin ...
... shows that the under - ground water- table at Jashpurnagar is about 30-45 ft . below the surface . At these depths the wells appear to have low recuperative powers . If , therefore , the site for the new well be selected in the doin ...
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Common terms and phrases
1.-General Report 3.-Mineral Production Aravalli Assam Baluchistan basal Bengal Bihar biotite Bombay calcareous Calcutta cassiterite Central Provinces charnockite Chinji Coal Coal-field conglomerate Congr Coulson Cretaceous Deccan trap deposits Dhok Pathan Diener district earthquake east Eastern Eastern States Agency Eocene F. R. C. Reed fauna felspar formation Fossil garnet genus Geol Geological Survey Geologist Geology gneisses gneissic Gondwana granite Hills Himalayas India intrusive Journ Kashmir limestone Lower Madras Memoir metamorphic meteorite Mica miles minerals Mining Miscellaneous Notes Nagpur Narbada North-West Northern Shan occur outcrops Paliyad Permian phyllites Pinjor plateau print).-Annual report Proc Production of India Punjab quartz quartzite Rajputana Red Beds river rocks rupees Sahni Salt Range sandstones schists shales sheet Siwalik Southern species specimens Surv Survey of India Tertiary Trias Triassic Twenty-fourth Ind Upper Burma valley veins Vindhyan VOL VOL Western wolfram Yunnan