Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 138
The evidence for a rupture on a gently dipping plane beneath the Shillong
Plateau in 1897 is too incomplete to neglect such a possibility . 5 April , 1905
Kangra earthquake Molnar and Deng ( 1984 ) did not discuss this event because
it ...
The evidence for a rupture on a gently dipping plane beneath the Shillong
Plateau in 1897 is too incomplete to neglect such a possibility . 5 April , 1905
Kangra earthquake Molnar and Deng ( 1984 ) did not discuss this event because
it ...
Page 148
The evidence reported above suggests relatively rapid vertical speeds of material
both in the Greater Himalaya and at the southern margin of the Lesser Himalaya ,
but similar evidence from most of the Lesser Himalaya is absent . Vertical ...
The evidence reported above suggests relatively rapid vertical speeds of material
both in the Greater Himalaya and at the southern margin of the Lesser Himalaya ,
but similar evidence from most of the Lesser Himalaya is absent . Vertical ...
Page 156
constant , but essentially no justification for this assumption is given in the
literature . In this paper we will consider recent evidence that normal stress
variations actually control the stick - slip process for both foam rubber and
earthquakes .
constant , but essentially no justification for this assumption is given in the
literature . In this paper we will consider recent evidence that normal stress
variations actually control the stick - slip process for both foam rubber and
earthquakes .
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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