Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 81
K - feldspar form anhedral xenocrysts that are mostly turbide and clouded . These
often enclose plagioclase which show intense alternation . Since this alternation
has caused the development of fractures in the enclosing k - feldspar grains ...
K - feldspar form anhedral xenocrysts that are mostly turbide and clouded . These
often enclose plagioclase which show intense alternation . Since this alternation
has caused the development of fractures in the enclosing k - feldspar grains ...
Page 93
AKP : Two - Feldspar Geothermometers Using Lotus 1-2-3 Software D.
RAMESHWAR RAO & T.V. SUBBA RAO Wadia Institute of Himalayan Geology ,
Dehra Dun - 248 001 , India Advance Data Processing Research Institute ...
AKP : Two - Feldspar Geothermometers Using Lotus 1-2-3 Software D.
RAMESHWAR RAO & T.V. SUBBA RAO Wadia Institute of Himalayan Geology ,
Dehra Dun - 248 001 , India Advance Data Processing Research Institute ...
Page 94
Whitney and Stormer ( 1977a ) have also produced a low - temperature
geothermometer for ordered K - feldspar . Their calibration estimates relatively
high temperatures in comparison to other geothermometers and is less
successful .
Whitney and Stormer ( 1977a ) have also produced a low - temperature
geothermometer for ordered K - feldspar . Their calibration estimates relatively
high temperatures in comparison to other geothermometers and is less
successful .
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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