Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 109
In the Lesser Himalaya also , the evapoirites occur in the Upper Riphaen
sequence ( Table 1 ) . However it seems that ... The first relatively longer and
more widespread , occurred from about 700 m.y. to about 600 to 625 m.y. ago .
The end ...
In the Lesser Himalaya also , the evapoirites occur in the Upper Riphaen
sequence ( Table 1 ) . However it seems that ... The first relatively longer and
more widespread , occurred from about 700 m.y. to about 600 to 625 m.y. ago .
The end ...
Page 137
N60 ° E AZIMUTH N30 ° E NOE N30 ° W 75 ° E 80 ° E 85 ° E 90 ° E 95 ° E the
corresponding east - west extension in southern Tibet does not require that
extension occurred by normal faulting ; conjugate strike - slip faulting in Tibet
could have ...
N60 ° E AZIMUTH N30 ° E NOE N30 ° W 75 ° E 80 ° E 85 ° E 90 ° E 95 ° E the
corresponding east - west extension in southern Tibet does not require that
extension occurred by normal faulting ; conjugate strike - slip faulting in Tibet
could have ...
Page 138
In any case , as Seeber and Armbruster ( 1981 ) suggested , I would not expect
the next great earthquake in the Himalaya to occur north of the Shillong Plateau .
At the same time , it probably would be unwise to design a program for seismic ...
In any case , as Seeber and Armbruster ( 1981 ) suggested , I would not expect
the next great earthquake in the Himalaya to occur north of the Shillong Plateau .
At the same time , it probably would be unwise to design a program for seismic ...
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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 |
28 other sections not shown
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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