Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 75
Lithofacies association Internal structure and contact relationship Biogenic
activity Thickness ( in metres ) Limestone 50 Thickly bedded ( massive in nature )
, base uneven Red and green shale Highly cleaved and crumpled 15 120
Limestone ...
Lithofacies association Internal structure and contact relationship Biogenic
activity Thickness ( in metres ) Limestone 50 Thickly bedded ( massive in nature )
, base uneven Red and green shale Highly cleaved and crumpled 15 120
Limestone ...
Page 195
The above - referenced paper indicate that the base of the Lower Cambrian
Tommotian Stage lies at or just below the base of the Tal Formation ; however ,
the recently ratified global stratotype section and point ( GSSP ) for the initial
Cambrian ...
The above - referenced paper indicate that the base of the Lower Cambrian
Tommotian Stage lies at or just below the base of the Tal Formation ; however ,
the recently ratified global stratotype section and point ( GSSP ) for the initial
Cambrian ...
Page 198
Processes ca 4um long and 3um wide at base . Remarks : Echinosphaeridium
maximum ( originally described as Baltisphaeridium maximum by Yin , 1987 ) is
common in parts of the Doushantuo Formation in China and additionally occurs
in ...
Processes ca 4um long and 3um wide at base . Remarks : Echinosphaeridium
maximum ( originally described as Baltisphaeridium maximum by Yin , 1987 ) is
common in parts of the Doushantuo Formation in China and additionally occurs
in ...
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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