Records of the Geological Survey of India, Volume 112, Part 3government of India., 1977 - Geology 1867- includes the "Annual report of the Geological survey of India". |
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Page 45
... traverse in a preferable direction was not of much significance due to low dips of the Barakar formations , the mi- nimum and the maximum lengths of traverses , were 50 and 300 m respectively . The lay - out of geophy- sical traverses ...
... traverse in a preferable direction was not of much significance due to low dips of the Barakar formations , the mi- nimum and the maximum lengths of traverses , were 50 and 300 m respectively . The lay - out of geophy- sical traverses ...
Page 45
... traverse T14 and from S11 to $ 55 on traverse T18 , these are considered stowed zones . Traverse T11 , near the tri - junction of Nayadih Kusunda , Pure Kustore and Godhur collieries ( Fig . 5 ) depicts the response over the boundary ...
... traverse T14 and from S11 to $ 55 on traverse T18 , these are considered stowed zones . Traverse T11 , near the tri - junction of Nayadih Kusunda , Pure Kustore and Godhur collieries ( Fig . 5 ) depicts the response over the boundary ...
Page 47
... traverse E6.4 is indicative of a probable fault zone in the vicinity of Sedirpara village . Resistivity profiles along traverse E32 over the broad gravity and magnetic anomaly zone near Jorabank have shown some fluctuations in ...
... traverse E6.4 is indicative of a probable fault zone in the vicinity of Sedirpara village . Resistivity profiles along traverse E32 over the broad gravity and magnetic anomaly zone near Jorabank have shown some fluctuations in ...
Contents
GEOLOGICAL SURVEY OF INDIA | 1 |
Some aspects of the geochemistry of Dhanjori Volcanics Singhbhum District | 7 |
Geology and Structure of Southern GangpurBonaigarh Region Sundargarh | 13 |
Copyright | |
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analysis andradite anomaly average axial plane Badampahar bands basin bauxite bedding Bihar biotite calc-gneiss chalcopyrite channel chlorite cleavage Colliery conglomerate Dalma deformation deposits Dhanjori epidiorite district dolerite dolerite dykes eastern epidiorite epidote F₁ facies fold fossils fractures fuchsite galena Gangpur Gangpur Group Geol Geological Survey geophysical Ghatsila gibbsite gneiss grains granite gneiss gravity Group-II rocks Hazaribagh hornblende indicate kaolinite Karharbari Formation Keonjhar Khola Kusunda laterite lavas limb lineation massive garnet metamorphic metasedimentary belt metres mica schists mineralisation minerals muscovite Nausahi Nayadih Kusunda occur Orissa pegmatite phyllite plagioclase Plate plunging quartz quartzite Raghunathpali Rajgir Rangpo Records regional resistivity samples sand sandstone saprolite Sarkar scale schist schistose sedimentary sediments sequence sericite shales shear shows Simlipal Singhbhum skarn stowed stress structures sulphide Sundargarh District Surv Survey of India syncline synformal textural thickness TRAV traverse trend ultrabasic rock unstowed volcanics Volume