Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 52
The intersection of bedding plane (SJ) and axial planes (S3, S4, and S5) have
been shown as B S3 S], I3 S SI, and B 853'(i) Mineral lineation g (ii) Lineation
due to intersection of S-planes (iii) Crenulation lineation (iv) Fold hinge lines
Mineml ...
The intersection of bedding plane (SJ) and axial planes (S3, S4, and S5) have
been shown as B S3 S], I3 S SI, and B 853'(i) Mineral lineation g (ii) Lineation
due to intersection of S-planes (iii) Crenulation lineation (iv) Fold hinge lines
Mineml ...
Page 54
Symmetry of Ijnear Fabrics The planes of schistosity and slaty cleavage which
are characterized by the orientation of mineral lineations and crenulation
lineations define a monoclinic symmetry 'Czh', where the lineation marks the 5:'
direction ...
Symmetry of Ijnear Fabrics The planes of schistosity and slaty cleavage which
are characterized by the orientation of mineral lineations and crenulation
lineations define a monoclinic symmetry 'Czh', where the lineation marks the 5:'
direction ...
Page 136
Oriattation of lineation (L ongaxis ofpebbler) and foliation plane (S 1) in the
conglomerate horizon of Sllagol melange alonglhe Indus-Tsango Suture Z one.
Location Structural No. of Contour % per Oriaitation Fig No No. Fabric
Obsavation Unit ...
Oriattation of lineation (L ongaxis ofpebbler) and foliation plane (S 1) in the
conglomerate horizon of Sllagol melange alonglhe Indus-Tsango Suture Z one.
Location Structural No. of Contour % per Oriaitation Fig No No. Fabric
Obsavation Unit ...
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Contents
Cnouasv KEWAL K SHARMA D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 21 |
G S MEHROTRA S SARKAR D P KANUNGO A geological appraisal of Landslide Hazards | 35 |
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Common terms and phrases
02:53 IST MAGNITUDE acanthomorphic acritarchs Agglomeratic Slate Amritpur axial plane Bafliaz Formation band basin biotite Budhal calcite chert classified clasts conglomerate defined deformation Dehra Dun deposits diamictite dolomite Doushantuo Formation Dum Gali Quartzite facies fault plane feldspar fi'om field figure fine first flank flows folds foliation fossils Garhwal Geol glacial gneiss granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation lndia lnfrakrol metamorphic Nappe ofthe Panjal thrust Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone schist sector sedimentary sediments sequence shale Sharma shear Shergol significance SiO2 slide slip slope soil stratigraphic structures Surv Suture Zone tectonic Tethyan Thakur thick Thinly bedded Uhl valley unconformably upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Zanskar