Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 17
That the activity has been spasmodic is reflected by submergence and
transgression during Permo - Carboniferous and the distribution of Panjal
volcanics both in the Zanskar and Kashmir - Chamba- Tandi basins lying to the
west of the PMZ .
That the activity has been spasmodic is reflected by submergence and
transgression during Permo - Carboniferous and the distribution of Panjal
volcanics both in the Zanskar and Kashmir - Chamba- Tandi basins lying to the
west of the PMZ .
Page 103
Both the types grade into one another and intrude into quartzites ( Bhim Tal
Formation ) and metabasics ( Bhowali Volcanics ) . Chemically , the granites and
porphyries show similar concentrations of major , minor , trace and LREE
elements .
Both the types grade into one another and intrude into quartzites ( Bhim Tal
Formation ) and metabasics ( Bhowali Volcanics ) . Chemically , the granites and
porphyries show similar concentrations of major , minor , trace and LREE
elements .
Page 104
The granites and porphyries occur as lensoid bodies in between Bhimtal
quartzites and Bhowali volcanics ( Fig . 1 ) and grade into one another thus
suggesting that both the rock types were emplaced simultaneously . They ( along
with their ...
The granites and porphyries occur as lensoid bodies in between Bhimtal
quartzites and Bhowali volcanics ( Fig . 1 ) and grade into one another thus
suggesting that both the rock types were emplaced simultaneously . They ( along
with their ...
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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