Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 46
The lower part of Shian quartzite represents fluvial environment indicating major
regressive phase . Silurian ( Pin dolomite ) marked the first major period of
carbonate accumulation followed by mudstone and sandstone facies . However ...
The lower part of Shian quartzite represents fluvial environment indicating major
regressive phase . Silurian ( Pin dolomite ) marked the first major period of
carbonate accumulation followed by mudstone and sandstone facies . However ...
Page 83
2 ) , with a major ocean still separating the arc from the Indian continent ( Pudsey
et al . , 1985 ; Petterson & Windley , 1985 ) . The major movement along the “
Northern Suture ” must post - date deposition of mid - Cretaceous limestones ...
2 ) , with a major ocean still separating the arc from the Indian continent ( Pudsey
et al . , 1985 ; Petterson & Windley , 1985 ) . The major movement along the “
Northern Suture ” must post - date deposition of mid - Cretaceous limestones ...
Page 88
25 their major elemental concentrations by XRF . The distribution of major
elements in different size grades of tailings and sludges are shown in Fig . 2 and
3 , respectively . 20TAILINGS 15 * 24 +0.0 PHI WEIGHT PERCENTAGE Fo20f %
2 -4.5 ...
25 their major elemental concentrations by XRF . The distribution of major
elements in different size grades of tailings and sludges are shown in Fig . 2 and
3 , respectively . 20TAILINGS 15 * 24 +0.0 PHI WEIGHT PERCENTAGE Fo20f %
2 -4.5 ...
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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