Journal of Himalayan Geology, Volume 3Wada Institute of Himalayan Geology, 1992 - Geology |
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Page 108
The fracture cleavage trends in (1) NNW-SSE and ENE-WSW directions and may
be due to F3 folding. Lineation The linear structure found in the Pokheri area has
been classed as follows: 'b ' lineation Packers: These are of three generations.
The fracture cleavage trends in (1) NNW-SSE and ENE-WSW directions and may
be due to F3 folding. Lineation The linear structure found in the Pokheri area has
been classed as follows: 'b ' lineation Packers: These are of three generations.
Page 114
They have been grouped under penetrative linear fabric, such as mineral
lineation, intersection lineations, crenulation lineation, fold hinge lines and
nonpenetrative linear fabric such as boudins, roddings and slickensides.
Penetrative linear ...
They have been grouped under penetrative linear fabric, such as mineral
lineation, intersection lineations, crenulation lineation, fold hinge lines and
nonpenetrative linear fabric such as boudins, roddings and slickensides.
Penetrative linear ...
Page 199
Lastly, in the northem portion we get clear evidences of folding with the fold axis
parallel to the strike of the thrust planes (Fig. 1; Section J). Mineral lineation
Mineral lineation is defined by the preferred dimensional orientation of inequant ...
Lastly, in the northem portion we get clear evidences of folding with the fold axis
parallel to the strike of the thrust planes (Fig. 1; Section J). Mineral lineation
Mineral lineation is defined by the preferred dimensional orientation of inequant ...
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Contents
Fold shape analysis in the vicinity of North Almora Thrust in District | 121 |
Simla group problem in HimalayaA critical review | 131 |
Geology of Kishanpur NagrotaBasantgarhGujru Nagrota Sector of Inner | 137 |
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Common terms and phrases
active Altyn Tagh fault Ambootia Armijo Arunachal axis beds belt Bhutan blocks Chail Chevron Folds complete carapace conglomerate deformation Deng displacement Dudatoli earthquake east-west fault plane solutions Gansser Garhwal Geol Geophys gneisses graben granite Hafla Haiyuan fault Himachal Pradesh Himalaya Himalayan Geology India Jammu region Jour Journal of Himalayan Ladakh landslide valley left-lateral slip limestone lineation lndia Lower Murree margin melange melange zone metamorphism mineral mm/a Murree mylonitic normal faulting offset ophiolitic ophiolitic melange orientation Peltzer phase phyllite Pokheri quartz quartzite right-lateral rocks roughly samples sandstones schist schistose section zone seismic Semi-Ellipses shale Shali shear Siddiqui Simla Simla group Simla Slates Sine Waves Singh Sinha Siwalik southern Tibet specimens strain strike-slip faulting structures Subathu Subathu Formation surface Surv Suture Zone syncline tectonic Tewari thrust faulting Tibet Tibetan Plateau trending turbidites Upper Murree Upper Siwalik valve view volcanics