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 17
... trend of this cleavage is N 40 ° E - S 40 ° W , dipping at 60 due northwest . The presence of a 5 % concentration of this cleavage dipping due southeast . might be due to a fanning in the axial zone of the fold . A second cleavage ...
... trend of this cleavage is N 40 ° E - S 40 ° W , dipping at 60 due northwest . The presence of a 5 % concentration of this cleavage dipping due southeast . might be due to a fanning in the axial zone of the fold . A second cleavage ...
Page 18
... trend , whereas in the axial zone , the dips are subvertical . The So has an average trend of N 80 ° E -S 80 ° W , dipping 46 ° due north in the southern limb ( Plate 3 - XIV ) and has an average trend of E - W dipping at a steep angle ...
... trend , whereas in the axial zone , the dips are subvertical . The So has an average trend of N 80 ° E -S 80 ° W , dipping 46 ° due north in the southern limb ( Plate 3 - XIV ) and has an average trend of E - W dipping at a steep angle ...
Page 31
... trend . The compressive stress of the later F2 deformation acted obliquely ( ′′ N108 ° ) to this trend and consequently , was resolved into a normal compressive stress and a shearing stress , pro- ducing a simple shear . The buckling of ...
... trend . The compressive stress of the later F2 deformation acted obliquely ( ′′ N108 ° ) to this trend and consequently , was resolved into a normal compressive stress and a shearing stress , pro- ducing a simple shear . The buckling of ...
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