Records of the Geological Survey of India, Volume 112, Part 8The Survey, 1977 - 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 95
... bedded kankar deposits occur in three longitudinal patches trending ENE - WSW and are separated by intervening sand dunal tracts . The average thickness of these deposits is 0.25 m under an overburden of about 0.80 m . Out of the total ...
... bedded kankar deposits occur in three longitudinal patches trending ENE - WSW and are separated by intervening sand dunal tracts . The average thickness of these deposits is 0.25 m under an overburden of about 0.80 m . Out of the total ...
Page 97
... BEDDED KANKAR General characters The lime - rich shelly bedded kankar deposit occurs on or at a very shallow depth of about a metre or so below the land surface . Exposures are mostly in ponds , locally know as Jorhs , such as east of ...
... BEDDED KANKAR General characters The lime - rich shelly bedded kankar deposit occurs on or at a very shallow depth of about a metre or so below the land surface . Exposures are mostly in ponds , locally know as Jorhs , such as east of ...
Page 103
... bedded kankar , the fragmentary kankar is concentrated along the palaeochannels on the gentle slopes flanking low - lying areas . Where the fragmentary kankar occurs , the bedded kankar is generally absent . In the sandy tract of the ...
... bedded kankar , the fragmentary kankar is concentrated along the palaeochannels on the gentle slopes flanking low - lying areas . Where the fragmentary kankar occurs , the bedded kankar is generally absent . In the sandy tract of the ...
Contents
RECORDS | 1 |
Geology Structure and Sulphide Mineralisation of Tosham District Bhiwani Haryana | 7 |
Geology and Geochemistry of Sulphide Mineralisation in Teejanwali Hill Mahendragarh | 17 |
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anomaly bands basin Bhander biotite calcareous Chail chemical comprises conglomerate Deoban belt Deoban Group depth Dharamsala Dharmigad district dunite dykes exposed fault fauna felspar folds foliation geochemical Geol Geological Survey Giri glacial glacier gneiss granite grey groundmass Haryana Himalaya ignimbrites Jamuna Jaunsar Jutogh Jutogh Thrust Kaimur Kallar kankar kankar deposits Kulu limestone Lower Main Central Thrust Mandhali Formation mapping metres mineralisation minerals Morar-Chakrata nala Narkasi Naugaon Nawagaon occur pebbles Permian phenocrysts phyllite plagioclase Plate-1 porphyroblastic porphyry Pradesh quartz quartzite Quaternary Raina Ramganga rhyolite river rocks Salnian samples sand Sandstone Sauli Formation schist schistose sediments sequence sericite Shale shear zone shelly bedded kankar silt siltstone Simla Siwalik slate slope soil Spiti stratigraphic structure Surv Survey of India Table-1 tectonic thickness tion Tiuni Tons valley Tosham hill Tr Tr trend tuff lavas Unpub Upper upto values Vindhyan volcanic Yamuna valley