Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 192
Rengging is another well known locality in the eastern part of the Siang region.
Nodular shales representing marine facies of the Gondwana Group and yielding
marine invertebrate fossils, are well developed around Rengging. Santra (1978)
...
Rengging is another well known locality in the eastern part of the Siang region.
Nodular shales representing marine facies of the Gondwana Group and yielding
marine invertebrate fossils, are well developed around Rengging. Santra (1978)
...
Page 192
Rengging is another well known locality in the eastern part of the Siang region .
Nodular shales representing marine facies of the Gondwana Group and yielding
marine invertebrate fossils , are well developed around Rengging . Santra ( 1978
) ...
Rengging is another well known locality in the eastern part of the Siang region .
Nodular shales representing marine facies of the Gondwana Group and yielding
marine invertebrate fossils , are well developed around Rengging . Santra ( 1978
) ...
Page 155
P. salinus is very significant . In the Indian Siwalik , the large number of Middle
Siwalik fossils are known only from Haritalyangar , Himachal Pradesh and this
locality is known for primate collection and dominant Nagri Fauna ( Vasishat et al
.
P. salinus is very significant . In the Indian Siwalik , the large number of Middle
Siwalik fossils are known only from Haritalyangar , Himachal Pradesh and this
locality is known for primate collection and dominant Nagri Fauna ( Vasishat et al
.
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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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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