Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 74
Fossils are rare and intraclast were also observed at certain levels Cherty
limestone is associated with limestone and is traversed by calcite veins . Fig . 11.
The caught up block of laminated limestone in the massive limestone in Aq Tash
...
Fossils are rare and intraclast were also observed at certain levels Cherty
limestone is associated with limestone and is traversed by calcite veins . Fig . 11.
The caught up block of laminated limestone in the massive limestone in Aq Tash
...
Page 75
... pisoidal limestone , cherty limestone , flaggy limestone and oolitic limestone .
Shale , siltstone , sandstone and conglomerate are also associated with
limestone . Limestone , in general , is light grey , thinly to thickly bedded and
shows sharp ...
... pisoidal limestone , cherty limestone , flaggy limestone and oolitic limestone .
Shale , siltstone , sandstone and conglomerate are also associated with
limestone . Limestone , in general , is light grey , thinly to thickly bedded and
shows sharp ...
Page 89
The associated anoxic facies and pelagic sediments indicate very deep marine
conditions . Volcanic episods in upper part followed by shallow marine deposits
indicate regression associated with rifting . The lower part of Saser Brangsa ...
The associated anoxic facies and pelagic sediments indicate very deep marine
conditions . Volcanic episods in upper part followed by shallow marine deposits
indicate regression associated with rifting . The lower part of Saser Brangsa ...
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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