Himalaya: Geological Aspects, Volume 2Contributed articles. |
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The strike of the dominant foliation is broadly N - S . Within this basement
sequence are infolded synclinal keels of a sedimentary and subordinate volcanic
cover sequence , with a marked unconformity and basal conglomerate , now ...
The strike of the dominant foliation is broadly N - S . Within this basement
sequence are infolded synclinal keels of a sedimentary and subordinate volcanic
cover sequence , with a marked unconformity and basal conglomerate , now ...
Page 151
The rock sequence in the Chamba - Bharmaur syncline , a part of Chamba nappe
( Thakur , 1998 ) , belong to Precambrian - Upper Palaeozoic age and is thrust
over the Lesser Himalayan Formations to the south along the Panjal thrust .
The rock sequence in the Chamba - Bharmaur syncline , a part of Chamba nappe
( Thakur , 1998 ) , belong to Precambrian - Upper Palaeozoic age and is thrust
over the Lesser Himalayan Formations to the south along the Panjal thrust .
Page 297
KUMAUN LESSER HIMALAYA Michael R.W. Johnson ABSTRACT The thrusts of
the Kumaun Lesser Himalaya evolved in a hinterland - to - foreland sequence in
which the Main Central ( " Vaikrita " ) thrust developed first , followed in time by ...
KUMAUN LESSER HIMALAYA Michael R.W. Johnson ABSTRACT The thrusts of
the Kumaun Lesser Himalaya evolved in a hinterland - to - foreland sequence in
which the Main Central ( " Vaikrita " ) thrust developed first , followed in time by ...
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Contents
The Central Himalayan Gneisses in Northern Pakistan | 1 |
LowPressure Metamorphism in a Regionally Metamorphic | 39 |
The Buniyar Granite of the Kashmir Himalaya | 61 |
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Almora angle appears assemblages associated augen axes axial axis bands base bedding belt biotite boundary Chail chlorite cleavage composition consists contain continuous crenulation crystalline deformation developed diagram direction District eastern exposed fabric facies faults folds foliation Formation formed fractures Garhwal garnet Geol Geology girdle gneiss grade grains granite Group higher Himalaya inclusions increase India indicate isograd Jour Jutogh Krol Kumaun kyanite Lesser Himalaya limestone lineation lower Main Central major metamorphism mica migmatites mineral movement muscovite mylonitic nappe Nepal observed occur orientation parallel pelitic phase phyllites plagioclase plane porphyroblasts present pressure quartz quartzite range reaction region relief represented result rocks Saklani schist schistosity sequence sericite sets shear sheet sillimanite similar Siwalik slates southern staurolite strain stratigraphic structural suggests surfaces Table tectonic temperature texture thickness thrust trend units upper valley West zone