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 94
... structural feature of the Murrees is the geniculate deflection at the crossing of the Biruin Nala where the strike of the rocks changes from N. W.-S. E. to N. E.-S. W. and later to E. by N.-W. by S. The cause of the bend is uncertain ...
... structural feature of the Murrees is the geniculate deflection at the crossing of the Biruin Nala where the strike of the rocks changes from N. W.-S. E. to N. E.-S. W. and later to E. by N.-W. by S. The cause of the bend is uncertain ...
Page 118
... Structural Studies in the Central Hima- laya , 1936. Himalayan Journ . , IX , 38-43 . ( c ) Tectonical Observations in the Central Himalaya of the Swiss Expedition , 1936 . International XVII Geological Congress , Abstracts of Papers ...
... Structural Studies in the Central Hima- laya , 1936. Himalayan Journ . , IX , 38-43 . ( c ) Tectonical Observations in the Central Himalaya of the Swiss Expedition , 1936 . International XVII Geological Congress , Abstracts of Papers ...
Page 155
... structural reason for the supposed limited solubilities between the two chief groups statistically detected by Boeke . All the garnets belong to the space - group 010 or Im3m which is the space - group of the highest degree of symmetry ...
... structural reason for the supposed limited solubilities between the two chief groups statistically detected by Boeke . All the garnets belong to the space - group 010 or Im3m which is the space - group of the highest degree of symmetry ...
Page 242
... structural relation between the minerals wolfram and cassiterite form more particularly along the walls and quartz predominates in the centre of the veins . The coarse bladed wolfram grew outwards from the vein walls , extending into ...
... structural relation between the minerals wolfram and cassiterite form more particularly along the walls and quartz predominates in the centre of the veins . The coarse bladed wolfram grew outwards from the vein walls , extending into ...
Page 248
... structural difference indicating boundary of the growth ring ( Pl . 15 , figs . 2 and 3 ) . However , at one extreme corner of the fossil , some suggestion of growth marks was noticed , which under a high 248 [ VOL . 73 . Records of the ...
... structural difference indicating boundary of the growth ring ( Pl . 15 , figs . 2 and 3 ) . However , at one extreme corner of the fossil , some suggestion of growth marks was noticed , which under a high 248 [ VOL . 73 . Records of the ...
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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