Records of the Geological Survey of India, Volume 59, Part 1The Survey, 1926 - Earthquakes |
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Page 19
... bands of granite . Between Phong - do Dzong and the capital city the rhyolite series was again crossed . ECONOMIC ENQUIRIES . Building Materials . See Limestone . Bee Limestone . Cement Materials . Coal . The authorities c 2 PART 1 ...
... bands of granite . Between Phong - do Dzong and the capital city the rhyolite series was again crossed . ECONOMIC ENQUIRIES . Building Materials . See Limestone . Bee Limestone . Cement Materials . Coal . The authorities c 2 PART 1 ...
Page 31
... bands amongst which is one prominent bed of purple shale . The lithological resemblance of certain of the beds to the basal nummulitic beds of the Pir Panjal and the occurrence in them of similar small fora- minifera , leave it hardly ...
... bands amongst which is one prominent bed of purple shale . The lithological resemblance of certain of the beds to the basal nummulitic beds of the Pir Panjal and the occurrence in them of similar small fora- minifera , leave it hardly ...
Page 32
... band to impound the water in this northern portion . The massive limestone in the places where it lies in its original bedding planes , that is to say , where it is not folded , appears to be reason- ably free from fissures , and its ...
... band to impound the water in this northern portion . The massive limestone in the places where it lies in its original bedding planes , that is to say , where it is not folded , appears to be reason- ably free from fissures , and its ...
Page 34
... bands , having an average thickness of about 60 feet , inter- bedded with softer silty sandstones and arenaceous clays occupying an average thickness of 20 feet between each band of massive sandstone . These beds belong to the upper ...
... bands , having an average thickness of about 60 feet , inter- bedded with softer silty sandstones and arenaceous clays occupying an average thickness of 20 feet between each band of massive sandstone . These beds belong to the upper ...
Page 35
... bands of massive sandstone , which form spurs jutting out into the river are , though soft , free from fissures and compact , and it is not anticipated that any danger is to be feared to that part of the line which may rest on this or ...
... bands of massive sandstone , which form spurs jutting out into the river are , though soft , free from fissures and compact , and it is not anticipated that any danger is to be feared to that part of the line which may rest on this or ...
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alluvium anticlines atacicus average Baluchistan Barakar beds Bhander Bihar and Orissa Bugti Bugti Hills Bundi Central Provinces Chhindwara district clays coal Coal-field conglomerate Cutch D'Archiac and Haime Deccan Trap deposits diameter Discocyclina dispansa Douvillé east Eocene equatorial section fault Fauna feet Fermor figs Foraminifera Fossil Geol Geological Survey Geology gneiss Gondwana granite Gwaliors Hills Himalayas horizon India Irrawadian javana Kashmir Kirthar series Laki series limestone locality Lower Kirthar Madras median chamber layer Memoir metamorphism Middle Kirthar miles Mineral Miscellaneous Notes Nagpur Nagpur district Nummulites Nuttall obtusus occur outcrops pegmatite Pegu Plate print).-Annual report Production of India Punjab quartz quartzites Rajputana river rocks Salt-range sandstone Sausar schists septal filaments shales Shan sheet Siwalik Sowerby species specimens strata stream structure surface Surv Tawa River Tertiary thickness unconformity Upper Burma Valley Vindhyan whorls Yamethin