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 36
Page 72
... ( Srikantia and Razdan , 1980a ) . However , considering its close tectonic association with the Permo - Trias Kuling - Lilang schuppen belt along its southern boundary , this must have developed as a conti- nental margin basin along the ...
... ( Srikantia and Razdan , 1980a ) . However , considering its close tectonic association with the Permo - Trias Kuling - Lilang schuppen belt along its southern boundary , this must have developed as a conti- nental margin basin along the ...
Page 80
... Srikantia , et al , 1978 ) . The Kuling - Lilang belt is often referred to as flysch ( Frank , et al , 1977 ) . However , the flysch nature is rather doubtful since the typical flyschoid character is rarely seen , excepting for local ...
... Srikantia , et al , 1978 ) . The Kuling - Lilang belt is often referred to as flysch ( Frank , et al , 1977 ) . However , the flysch nature is rather doubtful since the typical flyschoid character is rarely seen , excepting for local ...
Page 81
... ( Srikantia et al , 1978 ) . These volcanics are generally pahoehoe type and have aboundant pipe amygdules and ropy structure ( Srikantia , et al , 1978 ) . The Phe volcanics of Spiti- Zanskar are correlatable with Panjal volcanics of ...
... ( Srikantia et al , 1978 ) . These volcanics are generally pahoehoe type and have aboundant pipe amygdules and ropy structure ( Srikantia , et al , 1978 ) . The Phe volcanics of Spiti- Zanskar are correlatable with Panjal volcanics of ...
Contents
me Aspects of the Andaman Ophiolite Complex 111 | 1 |
phiolites of India 1354 | 29 |
Mass Susceptibility of Rocks of Brown Hill Indus Belt Ladakh 5559 | 55 |
Copyright | |
3 other sections not shown
Other editions - View all
Common terms and phrases
Andaman 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 emplaced Eocene facies flysch folded gabbro Gansser Geol Geological grains granite Granitoid green grey harzburgite Himalaya Indus Group Indus Ophiolite Belt Indus Suture Indus Tectonic Zone intrusive islands Kargil Karit Formation Kashmir Khardung Volcanics Kuksho Kuling-Lilang Ladakh Ladakh Granitoid Complex Ladakh Himalaya limestone mafic mafites magnetite mass susceptibility melange metamorphic mineral nala Nicobar Nidar Nindam Formation obducted occur oceanic crust olivine ophiolite ophiolite complex ophiolite nappe ophiolitic melange Pashkyum thrust peridotite pillow lavas plagioclase plagiogranite purple pyroxene 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 valley Zanskar