Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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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 .
Page 159
Brune ( 1973 ) , Archuleta and Brune ( 1975 ) , and Hartzell and Archuleta ( 1979
) observed stick - slip displacements of 5-10 cm and larger , on constrained
surfaces . A further check on the analogy with the Dieterich granite block results
is ...
Brune ( 1973 ) , Archuleta and Brune ( 1975 ) , and Hartzell and Archuleta ( 1979
) observed stick - slip displacements of 5-10 cm and larger , on constrained
surfaces . A further check on the analogy with the Dieterich granite block results
is ...
Page 164
The role of Normal Stress Variations in Stick - Slip Instabilities Background Many
recent studies in earthquake prediction and rock mechanics are based on the
analogy between earthquakes and stick / slip . Stick - slip has been observed in ...
The role of Normal Stress Variations in Stick - Slip Instabilities Background Many
recent studies in earthquake prediction and rock mechanics are based on the
analogy between earthquakes and stick / slip . Stick - slip has been observed in ...
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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