Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 109
This relationship is prominently marked when combined ferromagnesian
components ( FeO + Fe2O3 + MgO + Mno ) are plotted aganist silica and
suggests a process of fractional crystallisation in the granites and porphyries .
Components ...
This relationship is prominently marked when combined ferromagnesian
components ( FeO + Fe2O3 + MgO + Mno ) are plotted aganist silica and
suggests a process of fractional crystallisation in the granites and porphyries .
Components ...
Page 180
The waveforms on the left are for the parallel components , and on the right for
the parallel components . While full ... across the fault plane A u ( y , t ) may be
represented as a sum of a rupture component and a healing component as
follows .
The waveforms on the left are for the parallel components , and on the right for
the parallel components . While full ... across the fault plane A u ( y , t ) may be
represented as a sum of a rupture component and a healing component as
follows .
Page 188
In the cases of perpendicular components , the matches are best at Barkot ,
Ghansiali , and Purola . For the ... components of Ghansiali , the perpendicular
components at Tehri , and Koteshwar , and the parallel component at Barkot .
In the cases of perpendicular components , the matches are best at Barkot ,
Ghansiali , and Purola . For the ... components of Ghansiali , the perpendicular
components at Tehri , and Koteshwar , and the parallel component at Barkot .
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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 |
14 other sections not shown
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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