Records of the Geological Survey of India, Volume 107Geological Survey of India, 1972 - 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 49
... thickness of the individual bands normal to the bedding surface ( t ) and measurement of the angle x which the bedding makes with the horizontal line in the profile at each point in case of ten small scale fold specimens . The results ...
... thickness of the individual bands normal to the bedding surface ( t ) and measurement of the angle x which the bedding makes with the horizontal line in the profile at each point in case of ten small scale fold specimens . The results ...
Page 179
... thickness of the formation is about 5 metres . Babladanga Formation The type locality of this formation is to the east of Babladanga . This formation has a compactly cemented conglomerate at the base lying on the Archaean rocks . The ...
... thickness of the formation is about 5 metres . Babladanga Formation The type locality of this formation is to the east of Babladanga . This formation has a compactly cemented conglomerate at the base lying on the Archaean rocks . The ...
Page 180
... thickness of Bamundiha Formation is about 2 m . Bones of present day mammals occur in this formation with some incrusta- tions of lime . The bones are lighter as compared to those from the underlying horizons and do not show signs of ...
... thickness of Bamundiha Formation is about 2 m . Bones of present day mammals occur in this formation with some incrusta- tions of lime . The bones are lighter as compared to those from the underlying horizons and do not show signs of ...
Contents
A note on the polymetallic sulphide mineralisation in Askot area | 4 |
On studies of the Agglomeratic Slate and Panjal Trap in the Jhelum | 12 |
Chandranath granite Goa by A R Gokul and M D Srinivasan | 38 |
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acid agglomeratic slates amphibolite Archaean Ashtamudi assemblage Bababudan Group bands Barakar basalts basin beds Bihar biotite Boulder Conglomerate calcareous chelonian Chitradurga Chitradurga Group chlorite clays Coalfield craton Cuddapah deposits east epidote facies felspar folds fossil galena Geoclemys Geol Geological Survey Glossopteris Glossopteris flora gneisses gneissic complex Gondwana grained granite greenish grey greenstone belts high grade schists Hills Ibid indicated Karnataka Kashmir Kolar Kurnool lake laterite lead isotopic limestone lithological Lower Gondwana mafic Masumpur metamorphism mineralisation minerals non-porphyritic occur overlying Palaeobotanist Panjal trap pelitic phenocrysts Pichamuthu Pinjor Plate Plateau Pleistocene Pliocene porphyritic Precambrian pyroxene quartz quartzite Quilon Raniganj rock types Sandstone Sargur Supergroup schist schist belts schistose schistose rocks sediments sequence shales Siwalik stratigraphic studies Supergroup Surv Survey of India Sylhet Talchir Tatrot tectonic Tertiary thickness unconformity Upper upto valley Vindhyan volcanic Warkallis Western Block Zawar zeolite zone