Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
From inside the book
Results 1-3 of 50
Page 264
Sedimentology , petrography and tectonic significance of the shelf , flysch and
molasse clastic deposits across the Indus Suture Zone , Ladakh , N - W , India ,
Sediment . Geol . , 40 , 249-86 . DEWEY , J. F. , CANDE , S. & PITMAN , W. C.
1989.
Sedimentology , petrography and tectonic significance of the shelf , flysch and
molasse clastic deposits across the Indus Suture Zone , Ladakh , N - W , India ,
Sediment . Geol . , 40 , 249-86 . DEWEY , J. F. , CANDE , S. & PITMAN , W. C.
1989.
Page 1
This is generally considered to represent a suture zone , the Indus - Tsangpo
Suture , separating the Eurasian plate from the Indian plate since the Permian
time ( Srikantia , 1987 ) when fragmentation of the Gondwanaland occurred .
This is generally considered to represent a suture zone , the Indus - Tsangpo
Suture , separating the Eurasian plate from the Indian plate since the Permian
time ( Srikantia , 1987 ) when fragmentation of the Gondwanaland occurred .
Page 11
Initial subduction model is proposed along the Chillien Suture Zone in Central
China . A southward younging of subduction has been noticed . Under this
scheme , if the Shyok Zone is a subduction zone it represents an older
subduction than ...
Initial subduction model is proposed along the Chillien Suture Zone in Central
China . A southward younging of subduction has been noticed . Under this
scheme , if the Shyok Zone is a subduction zone it represents an older
subduction than ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
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
Other editions - View all
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