Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 94
Their calibration estimates relatively high temperatures in comparison to other
geothermometers and is less successful . However , they suggested that ,
reasonably accurate results may be obtained , by averaging their temperature
values with ...
Their calibration estimates relatively high temperatures in comparison to other
geothermometers and is less successful . However , they suggested that ,
reasonably accurate results may be obtained , by averaging their temperature
values with ...
Page 114
Rock / chondrite vs LREE plot for the rocks having average value of Sio ,
between 56-73 % , 73-75 % and more than 75 % . ... 100-1 10pro > 30 km 2.0 20-
30Km Log RD ROCK / ORG 15-20 km 1.0 0.1 15 km • Minimum values of the
Amritpur ...
Rock / chondrite vs LREE plot for the rocks having average value of Sio ,
between 56-73 % , 73-75 % and more than 75 % . ... 100-1 10pro > 30 km 2.0 20-
30Km Log RD ROCK / ORG 15-20 km 1.0 0.1 15 km • Minimum values of the
Amritpur ...
Page 185
... the noise variance for We take m = 0 and define R a priori subjectively as a
diagonal A m , o matrix with same value for ... is based on the idea that initial
model variance is inversely proportional to its corresponding information matrix
values .
... the noise variance for We take m = 0 and define R a priori subjectively as a
diagonal A m , o matrix with same value for ... is based on the idea that initial
model variance is inversely proportional to its corresponding information matrix
values .
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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