Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 43
The Kuling Formation as observed in different sections varies from 56 to 147.5
metres . The sandstone unit varies from 2 to 29 metres , whereas , shale unit
varies from 27 to 132.5 metres . This formation consists of sandstone ,
fossiliferous ...
The Kuling Formation as observed in different sections varies from 56 to 147.5
metres . The sandstone unit varies from 2 to 29 metres , whereas , shale unit
varies from 27 to 132.5 metres . This formation consists of sandstone ,
fossiliferous ...
Page 233
The maximum summits are observed in the basin ( 3005 m ) at the Dudhatoli
peak in the Upper Eastern - Western Nayar Interfluve in Dudhatoli - Khatil Water
Divide region and the minimum summits ( 1193 m ) occur in the Lower Nayar
Ganga ...
The maximum summits are observed in the basin ( 3005 m ) at the Dudhatoli
peak in the Upper Eastern - Western Nayar Interfluve in Dudhatoli - Khatil Water
Divide region and the minimum summits ( 1193 m ) occur in the Lower Nayar
Ganga ...
Page 129
The clay is almost uniform and only two episodes of higher concentration were
observed in the lower part ( Fig . 8 ) . The clay fraction in Attargo varies from 38.8
to 44.36 % . The textural classification of these samples and insoluble residue ...
The clay is almost uniform and only two episodes of higher concentration were
observed in the lower part ( Fig . 8 ) . The clay fraction in Attargo varies from 38.8
to 44.36 % . The textural classification of these samples and insoluble residue ...
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Contents
The Shyok valley Northern Ladakh India An entraped and compressed marginal | 1 |
Chemical mineralogy of the Panjal Traps around Bandipura Kashmir | 17 |
Structural characteristics of the rocks of BanihalRamban area | 23 |
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Common terms and phrases
activity associated authors basin beds belt biotite block Central correlation Crystallines deformation deposits developed District dolerite earthquakes eastern et al event exposed extends facies fault feldspars field folds followed Formation formed Garhwal Geol Geology gneisses grade grains granite granitoids Group higher Himalaya Himalayan Geology hornblende India indicate Indus Institute Jour Krol Ladakh Late later Lesser Himalaya limestone lower Main major margin material metamorphism Middle minerals nature Nayar northern observed occur oceanic ophiolitic origin phase phyllite plagioclase plane plate Pradesh present quartz quartzite range References region represented result river rocks Salt samples sandstone schist sedimentary sediments sequence Series shale Sharma Shyok Siwalik slip slope southern Spiti structural Subathu subduction suggests surface Suture Table tectonic thick Thrust trend units Upper valley values variation volcanics Wadia western zone