Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
From inside the book
Results 1-3 of 77
Page 17
... Folds of D , generation are overturned isoclinal folds of all sizes , folding the pre- Himalayan lithic banding or metamorphic layering . D1 folds , trending NW - SE , plunge due NW at low angles of about 10 to 12 degrees . D , folds ...
... Folds of D , generation are overturned isoclinal folds of all sizes , folding the pre- Himalayan lithic banding or metamorphic layering . D1 folds , trending NW - SE , plunge due NW at low angles of about 10 to 12 degrees . D , folds ...
Page 178
... folds are nearly coaxial . However , locally the hinge line of earlier folds show variation in their direction and amount of plunge due to refolding . The variations in the direction and amount of plunge of fold hinges of different ...
... folds are nearly coaxial . However , locally the hinge line of earlier folds show variation in their direction and amount of plunge due to refolding . The variations in the direction and amount of plunge of fold hinges of different ...
Page 27
... folds of later generations . B. Structure of second generation ( Fig . 5 ) ( i ) Open and asymmetrical folds often dishar- monic , polyclinal in style ( ii ) puckers with sharp hinge and kinks ( iii ) conjugate and box - like folds ( iv ) ...
... folds of later generations . B. Structure of second generation ( Fig . 5 ) ( i ) Open and asymmetrical folds often dishar- monic , polyclinal in style ( ii ) puckers with sharp hinge and kinks ( iii ) conjugate and box - like folds ( iv ) ...
Contents
RAJESH SHARMA B K NAYAK Ore petrology and origin of leadzinc deposits in great limestone | 103 |
R K MAZARI T N BAGATI Postcollision graben development in the Spiti valley Himachal | 111 |
P Dobhal SURENDAR KUMAR A K MUNDEPI Mass wasting and slope analysis of Chhota | 119 |
30 other sections not shown
Other editions - View all
Common terms and phrases
amphibolite Amritpur Amritpur Granite basin beds biotite block chlorite clasts conglomerate Cretaceous Crystallines deformation deposits developed dolerite dolomite earthquakes eastern Eocene evaporites facies fault feldspars folds fossils Garhwal Garhwal Himalaya garnet Geol glacial glacier gneisses Gondwana grained granitoids Group Himachal Pradesh Himalaya Himalayan Geology hornblende hornblende schists India Indian plate indicate Indus Suture Institute of Himalayan Jour Journal of Himalayan K-feldspar Krol Belt Kumar Kumaun Ladakh Lesser Himalaya limestone lineaments lithology lower magmatic margin metamorphism Middle Siwalik migmatites minerals Molnar moraines muscovite Nayar observed occur ophiolitic Ophiolitic Melange Pakistan phase phyllite plagioclase plane Precambrian quartz quartzite Rawat region river rocks Salt Range samples sandstone schist sedimentary sediments sequence shale Sharma shear zones shows Shyok Singh Siwalik slope Spiti stratigraphic structure Subathu Subathu Formation subduction Surv Suture Zone syncline tectonic Tethyan Thakur thick Thrust trend Upper Siwalik valley volcanics Wadia Institute western Zanskar