Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
From inside the book
Results 1-3 of 12
Page 72
These tear faults are nearly parallel to the great transform faults bounding the
Indian subcontinental block and some of the strikeslip faults recognized in the
Tibetan plateau and adjoining Chinese highlands ( Molnar & Tapponnier , 1975 ...
These tear faults are nearly parallel to the great transform faults bounding the
Indian subcontinental block and some of the strikeslip faults recognized in the
Tibetan plateau and adjoining Chinese highlands ( Molnar & Tapponnier , 1975 ...
Page 132
This convergence has continued , apparently unabated , since the collision ( e.g.
, Molnar & Tapponnier , 1975 ; Patriat & Achache , 1984 ; Powell , 1979 ) , with
different thrust faults in the Himalaya being active at different times . At present ...
This convergence has continued , apparently unabated , since the collision ( e.g.
, Molnar & Tapponnier , 1975 ; Patriat & Achache , 1984 ; Powell , 1979 ) , with
different thrust faults in the Himalaya being active at different times . At present ...
Page 153
MERCIER , J. L. , ARMIJO , R. , TAPPONNIER , P. , CAREY - GAILHARDIS , E. &
HAN TONG - LIN , 1987. Change from Late Tertiary compression to Quaternary
extension in southern Tibet during the IndiaAsia collision , Tectonics , 6 , 275-304
...
MERCIER , J. L. , ARMIJO , R. , TAPPONNIER , P. , CAREY - GAILHARDIS , E. &
HAN TONG - LIN , 1987. Change from Late Tertiary compression to Quaternary
extension in southern Tibet during the IndiaAsia collision , Tectonics , 6 , 275-304
...
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