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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Results 6-10 of 88
Page 66
... Evidence of faulting is seen in the Moulmein limestone exposures , but owing to their isolation in laterite , these effects are not visible the underlying rocks . Near Lutshan1 ( 15 ° Faulting . 48 97 ° 54 ′ ) , Mr. Leicester has ...
... Evidence of faulting is seen in the Moulmein limestone exposures , but owing to their isolation in laterite , these effects are not visible the underlying rocks . Near Lutshan1 ( 15 ° Faulting . 48 97 ° 54 ′ ) , Mr. Leicester has ...
Page 68
... evidence of having under- gone a considerably higher degree of metamorphism than those of the southern area . Mr. A. B. Dutt's main work consisted in the mapping of parts of sheets 93 C / 3 and 7 , C / 4 and 8 and D / 1 and 5. The ...
... evidence of having under- gone a considerably higher degree of metamorphism than those of the southern area . Mr. A. B. Dutt's main work consisted in the mapping of parts of sheets 93 C / 3 and 7 , C / 4 and 8 and D / 1 and 5. The ...
Page 78
... evidence of the beds of the Sylhet limestone stage north of a line joining Pyngkerdem ( 25 ° 21 ′ : 91 ° 54 ′ ) and Sohrarim . Mr. V. R. R. R. Khedker , Assistant Geologist , left for the field on the 3rd February 1937 , for the Garo ...
... evidence of the beds of the Sylhet limestone stage north of a line joining Pyngkerdem ( 25 ° 21 ′ : 91 ° 54 ′ ) and Sohrarim . Mr. V. R. R. R. Khedker , Assistant Geologist , left for the field on the 3rd February 1937 , for the Garo ...
Page 88
... evidence of much folding in the Tanawals in the higher reaches of the Ferozpur Nala and the increased width of outcrop is due to repetition by folding . The Tanawals extend southwards into Punch and north - west into the Uri district ...
... evidence of much folding in the Tanawals in the higher reaches of the Ferozpur Nala and the increased width of outcrop is due to repetition by folding . The Tanawals extend southwards into Punch and north - west into the Uri district ...
Page 104
... evidence , for similar rocks also occur in the Upper Gondwana formation . The base of the formation is nowhere clearly seen but there is little doubt that it rests directly on the eroded surface of the Archæans . These rocks are ...
... evidence , for similar rocks also occur in the Upper Gondwana formation . The base of the formation is nowhere clearly seen but there is little doubt that it rests directly on the eroded surface of the Archæans . These rocks are ...
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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