Records of the Geological Survey of IndiaGeological Survey of India, 1887 - 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 2
... probably of the same age as that of Bundel- khand ( Manual , p . 21 ) . Mr. Foote resumed his survey in Bellary at the beginning of the current season , but he has since been deputed to report on some gold - fields in Mysore , at the ...
... probably of the same age as that of Bundel- khand ( Manual , p . 21 ) . Mr. Foote resumed his survey in Bellary at the beginning of the current season , but he has since been deputed to report on some gold - fields in Mysore , at the ...
Page 4
... probably some unconformity , for the massive quartzite is locally in contact with different rocks of the underlying series ; this , however , might be due to faulting where the strata are so greatly disturbed . The gradual change from ...
... probably some unconformity , for the massive quartzite is locally in contact with different rocks of the underlying series ; this , however , might be due to faulting where the strata are so greatly disturbed . The gradual change from ...
Page 9
... probably including some converted paleozoics , were taken to be largely made up of older ( ? archæan ) gneiss , the continuation of that forming the Ladak axis . Dr. Giles does not pretend to be a geologist , but he made some excellent ...
... probably including some converted paleozoics , were taken to be largely made up of older ( ? archæan ) gneiss , the continuation of that forming the Ladak axis . Dr. Giles does not pretend to be a geologist , but he made some excellent ...
Page 17
... probably post - cretaceous age amongst which syenitic granite and traps are most conspicuous . The lines of fissure correspond generally with the direction of the anticlinals , although at several points the reverse is clearly seen ...
... probably post - cretaceous age amongst which syenitic granite and traps are most conspicuous . The lines of fissure correspond generally with the direction of the anticlinals , although at several points the reverse is clearly seen ...
Page 18
... probably by a system of parallel flexures , which result in a series of separate ranges as it were , but the structure is greatly obscured by intrusive igneous rocks , chiefly hornblendic granite , which has altered the neighbouring ...
... probably by a system of parallel flexures , which result in a series of separate ranges as it were , but the structure is greatly obscured by intrusive igneous rocks , chiefly hornblendic granite , which has altered the neighbouring ...
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Common terms and phrases
Afghanistán anticlinals appears augite Bág Band Bawar beds belong Blaini Blanford Bose boulders Calcutta carboniferous Cenomanian character Chirákhán Chor clay closely allied coal Coal-field colour conglomerate crystalline crystals Deccan traps deposits Dudatoli east eocene feet felspar Flsc foliation fossils fragments genus Geol Geological Survey gneiss gneissose granite Gondwana Haibak hills Himalayas Hindu Kush horizon hornblende igneous rocks Indian Museum Jaunsar jurassic Kúsh latter limestone lower magnetite mandible Marl metamorphism mica microscope miles mineral miocene molars namadicus neocomian numerous nummulitic occur outcrop Outer formations palæindicus Perim Island pliocene porphyritic present Punjab quartz quartzites range ridge river Royal 8vo sandstone schistose schistose series schists seam seen shales Simla sivalensis Siwalik slates slices Society species specimens strata stream structure Survey of India tertiary thickness traps Turán Turkistán unconformity upper cretaceous valley volcanic XVII XVIII
Popular passages
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Page 203 - ... or a granite-porphyry ; when, in the course of the earth-movements that were contorting, crumpling, and folding the strata of the Himalayas, this imperfectly consolidated graniteporphyry was forced through the faults that had been formed along the axes of over thrust-folds ; the semi-plastic mass was subjected to enormous pressure ; the mica was crumpled ; the crystals of felspar were cracked and ruptured...