Records of the Geological Survey of India, Volume 112, Part 7The Survey, 1982 - 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 27
... considered the Banded Gneissic Complex and the Bundelkhand Gneiss as the basement for the sequence of rocks lying in between them and assigned them to the Aravalli System . However , Saxena ( 1966 ) suggested that these gneisses should ...
... considered the Banded Gneissic Complex and the Bundelkhand Gneiss as the basement for the sequence of rocks lying in between them and assigned them to the Aravalli System . However , Saxena ( 1966 ) suggested that these gneisses should ...
Page 95
... considered to be responsible for mineralisation . No such relationship , however , is directly evident in the Zawar and Rajpura - Dariba mineralised zones , which are stratiform deposits . The lineaments in these two areas are considered ...
... considered to be responsible for mineralisation . No such relationship , however , is directly evident in the Zawar and Rajpura - Dariba mineralised zones , which are stratiform deposits . The lineaments in these two areas are considered ...
Page 98
... considered to be stratiform but evidences of epigenetic origin are also recorded . Khetri region Within this region are located more than three dozen small to medium sized deposits in an extent of more than 80 km from Ragunathgarh in ...
... considered to be stratiform but evidences of epigenetic origin are also recorded . Khetri region Within this region are located more than three dozen small to medium sized deposits in an extent of more than 80 km from Ragunathgarh in ...
Contents
Coastal geomorphology of Bhavnagar Gujarat India O | 1 |
Sediments of river Mendhaan admixture of humid and arid epoch | 11 |
CONTENTS | 16 |
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Ajabgarh Group albite Alwar Group Aravalli Aund axial Banded Gneissic Complex Bari Sadri basin Bayana beds Berach Granite Bhadesar Bhavnagar biotite Buchara Bundelkhand Gneiss calcite chert chlorite colour conglomerate country rocks cross-bedding Delhi Delhi Supergroup deposits district dolomite east eastern emplacement epidote facies fault felsite felspar felspathic ferruginous folds foliation fractures Geol Geological Survey geosynclinal cycle Gneiss grade grains of quartz granite porphyry grey Gujarat hornblende intrusive Jahaj Jaipur Jogipura Formation Khardeola Khareri Khetri Kushalgarh Kutch limestone magmatic matrix metamorphism metasediments mica schist microcline migmatites mineralisation minerals muscovite NE-SW Nithar northeastern Rajasthan occur oligoclase oolites orthoclase pebbles pegmatite phase phenoclasts phyllites places Pre-Aravalli pre-Delhi quartz quartz felsite quartzite Raialo Rajasthan ripple marks Salenia sand sandstone schist sedimentary sedimentation seen sequence sericite shale shows siliceous Sita slates specimen stratigraphic Supergroup surface Surv Survey of India tectonic terrace thick trend unconformity veins Vindhyan western zone