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 63
Page 46
... thin . The possibi- lity , therefore , of a deep reservoir of water existing in this area , suitable for extensive irrigation , is considered by Mr. West to be out of the question . Nindeh reservoir dam site , Mirzapur dis- trict , U ...
... thin . The possibi- lity , therefore , of a deep reservoir of water existing in this area , suitable for extensive irrigation , is considered by Mr. West to be out of the question . Nindeh reservoir dam site , Mirzapur dis- trict , U ...
Page 48
... thin skin over Dharwar schists . Between these two main formations is a variable thickness of gravel and clay which probably represent the Lameta beds of other parts of India . The present water supply is derived from numerous wells ...
... thin skin over Dharwar schists . Between these two main formations is a variable thickness of gravel and clay which probably represent the Lameta beds of other parts of India . The present water supply is derived from numerous wells ...
Page 61
... thin bands richer in biotite are almost schistose , and white bands consist almost entirely of tourmaline , quartz , and felspar . Sometimes a fine - grained biotite - muscovite gneiss occurs in associa- tion with the tourmaline granite ...
... thin bands richer in biotite are almost schistose , and white bands consist almost entirely of tourmaline , quartz , and felspar . Sometimes a fine - grained biotite - muscovite gneiss occurs in associa- tion with the tourmaline granite ...
Page 77
... thin out in a northerly direction and cannot be identified north of Laitryngew ( 25 ° 24 ′ 91 ° 56 ' ) . On the Thang Jnat plateau Mr. Ghosh has found that the Cherra sandstone , which succeeds the Cretaceous , ends near Ryngain ( 25 ...
... thin out in a northerly direction and cannot be identified north of Laitryngew ( 25 ° 24 ′ 91 ° 56 ' ) . On the Thang Jnat plateau Mr. Ghosh has found that the Cherra sandstone , which succeeds the Cretaceous , ends near Ryngain ( 25 ...
Page 79
... thin irregular laminations of sericite and show current bedding . Those which are towards the west of the slates however have more sericite and are often foliated . ( 4 ) Between Mawiong ( 25 ° 34 ' 91 ° 43 ′ ) and Nongti ( 25 ° 33 ...
... thin irregular laminations of sericite and show current bedding . Those which are towards the west of the slates however have more sericite and are often foliated . ( 4 ) Between Mawiong ( 25 ° 34 ' 91 ° 43 ′ ) and Nongti ( 25 ° 33 ...
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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