Records of the Geological Survey of India, Volume 115Geological Survey of India, 1985 - Earthquakes 1867- includes the "Annual report of the Geological survey of India". |
From inside the book
Results 1-3 of 46
Page 69
... thick sequence of Jurla Member with a purple coarse grit sandstone about 0-100m thick succeeded by thick bedded green - grey n : dium to coarse - grained sandstone . The upper part is haracterised by rhythmically repeated sequence of ...
... thick sequence of Jurla Member with a purple coarse grit sandstone about 0-100m thick succeeded by thick bedded green - grey n : dium to coarse - grained sandstone . The upper part is haracterised by rhythmically repeated sequence of ...
Page 71
... thick sequence of shale , siltstone , graywacke sandstone , quartz - arenite , subordinate limestone and diamictite in the type area ( Srikantia and Razdan , 1980a ) . In the sector of Shergol - Lungkerche , the Nindam Formation is ...
... thick sequence of shale , siltstone , graywacke sandstone , quartz - arenite , subordinate limestone and diamictite in the type area ( Srikantia and Razdan , 1980a ) . In the sector of Shergol - Lungkerche , the Nindam Formation is ...
Page 75
... thick sequence of sediments which succeedes the Dras Volcanic Formation ( Srikantia and Razdan , 1980a ) . Where the Dras Volcanics are not developed as in the wide central sector , the Nindam sediments directly overlie the Khalsi ...
... thick sequence of sediments which succeedes the Dras Volcanic Formation ( Srikantia and Razdan , 1980a ) . Where the Dras Volcanics are not developed as in the wide central sector , the Nindam sediments directly overlie the Khalsi ...
Contents
Ophiolites of India 1354 | 13 |
Mass Susceptibility of Rocks of Brown Hill Indus Belt Ladakh M4 5559 | 55 |
On the Geology and Tectonics of part of Central Ladakh Region | 61 |
2 other sections not shown
Other editions - View all
Common terms and phrases
Andaman-Nicobar assemblage associated bands basalt basin batholith beds characteristic chert chlorite chromite chromitite clasts composition comprises conglomerate Cretaceous crystalline cumulate diabase diorite Dras Volcanic Formation dunite dyke swarms eastern emplaced Eocene facies flysch folded gabbro Gansser Geol grains granite Granitoid green grey harzburgite Himalaya Indus Indus Group Indus Ophiolite Belt Indus Suture Indus Tectonic Zone intrusive Kargil Karit Formation Kashmir Khalsi Formation Khardung Volcanics Kuksho Kuling-Lilang Ladakh Ladakh Granitoid Complex Ladakh Himalaya limestone mafic mafic suite mafites magnetite metamorphic mineral nala Nicobar islands Nindam Formation obducted occur oceanic crust olivine ophiolite ophiolite complex ophiolitic melange overlying Pashkyum thrust peridotite pillow lavas plagioclase plagiogranite purple pyroxene represents Rutland Island samples sandstone Sangeluma belt Sangeluma Group schist schuppen sector sedimentary sediments sequence serpentine serpentinite shale sheared Shergol Formation Shyok siltstone spilite Srikantia and Razdan Surv Survey of India Suture Zone texture thick trend ultramafic ultramafites upper Zanskar