Records of the Geological Survey of India, Volume 120, Parts 2-8government of India., 1985 - 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. |
From inside the book
Results 1-3 of 3
Page 55
... Pleistocene to present . Four series of strandlines identified in the area probably developed during Holocene period . The average rate of progradation of the delta during the Holocene along the Krishna river is 3.34 m / year . The ...
... Pleistocene to present . Four series of strandlines identified in the area probably developed during Holocene period . The average rate of progradation of the delta during the Holocene along the Krishna river is 3.34 m / year . The ...
Page 56
... Pleistocene - early Holocene . The palaeochannels are identified on the basis of vegetation , alluvial facies and ground water occurrence . They are favour- able for shallow ground water developement . A levee over a width of one ...
... Pleistocene - early Holocene . The palaeochannels are identified on the basis of vegetation , alluvial facies and ground water occurrence . They are favour- able for shallow ground water developement . A levee over a width of one ...
Page 59
... Pleistocene underlying the modern delta . The geomorphic evolutionary growth of the different sectors of the delta might indi- cate that the inner western delta developed ear- lier to the northern delta . The eastern delta is the ...
... Pleistocene underlying the modern delta . The geomorphic evolutionary growth of the different sectors of the delta might indi- cate that the inner western delta developed ear- lier to the northern delta . The eastern delta is the ...
Contents
Contents | 1 |
Stratigraphy and structure of Delhi Supergroup of rocks | 12 |
Structures in Singhbhum shear zone at and around | 27 |
Copyright | |
2 other sections not shown
Other editions - View all
Common terms and phrases
anhydrite antiform Aravalli range average axial planes bands Barotiya and Sendra Barotiya Group basalts basin Bhim Group block boreholes Chaibasa channel chert Chitradurga chlorite clay crescentic lamina deformation Delhi Delhi Supergroup deposit developed Devgarh Devgarh Group dextral Dhanjori drilling east eastern evaporites exploration F₂ folds folds F formation Geol Geological map geophysical gneiss gold grade granite gravity ground water halite Haryana hinge Hutti Ingaldhalu iron isoclinal Jodhpur laterite limb lineation lode metabasalts metamorphism migmatization mineral mineralisation minor folds Nagaur occur phase of folding planar plunge polyhalite pre-Delhi inlier pre-Delhi west Precambrian Punjab quartz quartzite Rajasthan Rajgarh Rajgarh Group Ras Marble red beds regional rocks Rohtak district samples schist schist belt schistosity sediments Sendra Group sequence shear zone Singhbhum strand plain stratigraphic Strike Reef structures sulphide Supergroup Surv Survey of India synform tectonic thickness tion trend Tuff values variogram Vasudev volcanics western