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Page 136
4 : Generalised section between Simla and Rupshu (Modified after A. Berthelsen,
I951 and adopted from Saxena. I971 b). '<9 oun GRAVELS /1,0 ta 4') )1va 4_
cumorua \\ Wm “L N E SW 'loge "WWI-'I'¢ LOWER nt 1" ' Q, ' ' 4 a rgtrtm KROL ...
4 : Generalised section between Simla and Rupshu (Modified after A. Berthelsen,
I951 and adopted from Saxena. I971 b). '<9 oun GRAVELS /1,0 ta 4') )1va 4_
cumorua \\ Wm “L N E SW 'loge "WWI-'I'¢ LOWER nt 1" ' Q, ' ' 4 a rgtrtm KROL ...
Page 138
The crystalline basement below Simla Slate is not exposed. ln southeast Kashmir
, Chamba-Pangi, Spiti and North Kumaun, the sedimentary thicknesses on the
sloping extensions of the crystalline continental basement are about 8, S00 m, 5,
...
The crystalline basement below Simla Slate is not exposed. ln southeast Kashmir
, Chamba-Pangi, Spiti and North Kumaun, the sedimentary thicknesses on the
sloping extensions of the crystalline continental basement are about 8, S00 m, 5,
...
Page 142
Srikantia and Bhargava (I974) considered Jaunsar as a separate 'Group' and
Simla as a separate 'Group'. According to these authors the 'Jaunsar Group'
represents typical eugeosynclinal type sediments deposited on the eroded
surfaces of ...
Srikantia and Bhargava (I974) considered Jaunsar as a separate 'Group' and
Simla as a separate 'Group'. According to these authors the 'Jaunsar Group'
represents typical eugeosynclinal type sediments deposited on the eroded
surfaces of ...
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Contents
Tectonics and Structure of the Pamirs | 9 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 19 |
Peninsular and Himalayan Precambrian Belts | 31 |
Copyright | |
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Common terms and phrases
Acharyya Alpine Alps associated basement faults basin batholith belt biotite Bordet Central Crystalline collision continental Cretaceous crust crustal deformation deposits Earth Planet earthquakes Eastem Eocene facies field first flow flysch folds foreland formation Gansser Garhwal Geodynamics Geol Geology Geophys geosyncline gneiss Gondwana granite Himalaya Indian plate Indus island arc Jour Karakorum Kashmir Klootwijk Krol Kumaun Ladakh Late Lesser Himalaya limestone lndus Lower magmatic Main Boundary Main Central Thrust margin melange Mesozoic metamorphism Molnar movement nappe Nepal northem occur oceanic ofthe ophiolite orogenic Pakistan Palaeogene palaeomagnetic Palaeozoic Pamir Pande Panjal phase plate tectonics Plateau Precambrian Proterozoic quartzite Quetta Range region rocks rotation Saklani sandstones Saxena schists sedimentary sediments seismicity sequence serpentinite significance Simla Siwalik southem stratigraphic structural subduction Surv suture zone Tectonic Zone Tectonophysics Tertiary Tethyan Tethys thickness Tibetan slab Upper Valdiya volcanics westem