Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 15
The fauna and lithology indicate that the rocks have close affinity with the
Kashmir - Chamba - Bhalesh Tethyans rather than the Lahaul - Spiti - Tethyans
which lie only 25-30 km away . This indicates that the Tandi transgression was
from the ...
The fauna and lithology indicate that the rocks have close affinity with the
Kashmir - Chamba - Bhalesh Tethyans rather than the Lahaul - Spiti - Tethyans
which lie only 25-30 km away . This indicates that the Tandi transgression was
from the ...
Page 89
The faunal assemblages recorded from the member 2 of Burtsa Formation
indicates Lias Campanian age . The upper member ... The associated anoxic
facies and pelagic sediments indicate very deep marine conditions . Volcanic
episods in ...
The faunal assemblages recorded from the member 2 of Burtsa Formation
indicates Lias Campanian age . The upper member ... The associated anoxic
facies and pelagic sediments indicate very deep marine conditions . Volcanic
episods in ...
Page 91
During lower to Middle Triassic the deeper water facies assemblage is indicated
by geometry , facies and microfacies ... geometry of sediments and microfacies
assemblage indicate tidal to deep water and lagoonal facies- asemblage .
During lower to Middle Triassic the deeper water facies assemblage is indicated
by geometry , facies and microfacies ... geometry of sediments and microfacies
assemblage indicate tidal to deep water and lagoonal facies- asemblage .
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Contents
Petrogenesis of the Granitoid Rocks Chor Region Himachal Himalaya | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
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Common terms and phrases
Agglomeratic Slate analysis associated band base basin bedded belt chert components composition comprising conglomerate contain covered deformation Dehra deposits developed direction distribution district earthquake et al exposed facies fault fault plane feldspar field folds foliation followed Formation fossils Garhwal Geol gneiss grained granites granitoids grey Group higher Himalaya Himalayan Geology India indicates inversion Jour Kashmir Ladakh Lamayuru Late Lesser limestone lineation locality locations lower major Member metamorphic minerals observed occur Panjal pebbles phase phyllites plagioclase plane Pleistocene porphyries present quartz quartzite range region reported represented river road rocks samples sandstone schist sector sedimentary sediments sequence shale Sharma shown Slate slide slip slope soil strain stratigraphy strike structures suggest Surv Table tectonic thick thrust trace unit upper valley VALUES Volcanics Wadia weathered Zanskar zone