Records of the Geological Survey of India, Volume 128, Part 7The Survey, 1998 - 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 1
... folds ( F2 ) with a NW - SE trending fold axis . These folds show upright geometry at the eastern part of the area and gradually become overturned towards west . A pervasive schistosity ( S2 ) , axial planar to these folds , is the most ...
... folds ( F2 ) with a NW - SE trending fold axis . These folds show upright geometry at the eastern part of the area and gradually become overturned towards west . A pervasive schistosity ( S2 ) , axial planar to these folds , is the most ...
Page 14
... folds , with varying plunges and bearings . The folds of second phase ( F2 ) are asymmetrical , open to overturned with easterly dipping 50 to 60 ° axial plane plunging due NNE or SSW . The F2 and F , folds are coaxial . The F , folds ...
... folds , with varying plunges and bearings . The folds of second phase ( F2 ) are asymmetrical , open to overturned with easterly dipping 50 to 60 ° axial plane plunging due NNE or SSW . The F2 and F , folds are coaxial . The F , folds ...
Page 33
... folds are developed on the limbs whereas parasitic " M " - and " W " -shaped folds are noticed in the hinge zones of these F2 folds . The plunge of these folds varies from 25 to 75 ° towards S and SE as well as towards N and NE . The ...
... folds are developed on the limbs whereas parasitic " M " - and " W " -shaped folds are noticed in the hinge zones of these F2 folds . The plunge of these folds varies from 25 to 75 ° towards S and SE as well as towards N and NE . The ...
Contents
Investigation for base metals in Katar area Udaipur district Rajasthan | 21 |
Integrated geophysical surveys in SinghanaMoradpurPacheri | 27 |
Integrated multidisciplinary programme of search | 34 |
Copyright | |
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Common terms and phrases
Agucha Ajmer district amphibolite anomaly Aravalli Supergroup Banas bands Banswara district basalt base metal basement basin Bhilwara Bhukia Bikaner district boreholes calc-silicate rocks carried chalcopyrite Champaner Champaner Group Chitar comprises core samples Dariba Dariba-Bethunmi Debari delineated Delwara deposit depth dolomite drilling Dungarpur district evaluate exploration exposed Fold Belt Formation foundation grade galena geochemical sampling geological mapping geophysical surveys geotechnical investigations gneisses Gneissic granite groundwater Gujarat indicated intersected irrigation Jodhpur district Kalab Khandia km² area limestone lithounits Lower Lunavada Lunavada Group Mangalwar Complex metamorphism metasedimentary mica schist migmatites mineralised zones minerals North Sindesar Ridge occur Pb-Zn mineralisation phases of deformation phyllite Pipaliya Pipela Project pyrite pyrrhotite quartz veins quartzite Rajasthan Rajsamand Rajsamand district regional river sandstone Sawar schist sediments sequence shear soil strike length structure studies sub-block sulphide mineralisation Supergroup surface thematic mapping thick Toposheet transect trending Udaipur Udaipur district Upper