Records of the Geological Survey of India, Volume 115Geological Survey of India, 1980 - Earthquakes 1867- includes the "Annual report of the Geological survey of India". |
From inside the book
Results 1-3 of 24
Page 83
... ultramafic rocks . The ultramafic rocks occur as larger boudins , lenticular bodies , long tapering lenses within the Shergol sediments . These bodies are dark green and dark greenish grey in colour and very in dimensions on an average ...
... ultramafic rocks . The ultramafic rocks occur as larger boudins , lenticular bodies , long tapering lenses within the Shergol sediments . These bodies are dark green and dark greenish grey in colour and very in dimensions on an average ...
Page 95
... ultramafic rocks : are seen near Stargiuksa in the western part of the area , in the Khalsar - Diskit road section , and further east in Darbuk area near Tsoltak . Lenses of ultramafic rocks are also seen along the Shyok lineament near ...
... ultramafic rocks : are seen near Stargiuksa in the western part of the area , in the Khalsar - Diskit road section , and further east in Darbuk area near Tsoltak . Lenses of ultramafic rocks are also seen along the Shyok lineament near ...
Page 96
... ultramafic zone is overlain by basalts and pillow lavas . The ultramafic rocks of this zone are mostly serpen- tinitic with patches of unaltered rocks consisting of dunite and peridotite . These occur in a long , narrow , linear bodies ...
... ultramafic zone is overlain by basalts and pillow lavas . The ultramafic rocks of this zone are mostly serpen- tinitic with patches of unaltered rocks consisting of dunite and peridotite . These occur in a long , narrow , linear bodies ...
Contents
ome Aspects of the Andaman Ophiolite Complex 111 | 1 |
phiolites of India 1354 | 13 |
Hass Susceptibility of Rocks of Brown Hill Indus Belt Ladakh 5559 | 55 |
3 other sections not shown
Other editions - View all
Common terms and phrases
Andaman antiform assemblage associated bands basalt basin batholith beds Biagdang Formation chert chlorite chromite chromitite clasts composition comprises conglomerate Cretaceous crystalline cumulate diabase diorite Dras Volcanic Formation dunite dyke eastern emplaced Eocene facies flysch folded gabbro Gansser Geol grains granite Granitoid green grey harzburgite Himalaya 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 mafites magnetite mass susceptibility melange metamorphic mineral nala Nindam Formation obducted occur oceanic crust olivine ophiolite ophiolite complex ophiolite nappe ophiolitic melange Pashkyum thrust peridotite pillow lavas plagioclase plagiogranite purple pyroxene pyroxenite represents samples sandstone Sangeluma belt Sangeluma Group schist schuppen sector sedimentary sediments sequence serpentine serpentinite shale sheared Shergol Formation Shyok siltstone spilite Spiti Srikantia and Razdan Surv Survey of India Suture Zone texture thick trend ultramafic ultramafites Zanskar