Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 82
... dolomite are dominant minerals wheareas ferroan calcite is dominant in few microfacies . Ferroan dolomite is generally present in veins , voids and pore spaces . Quartz is main detrital followed by feldspar . The extraclast include ...
... dolomite are dominant minerals wheareas ferroan calcite is dominant in few microfacies . Ferroan dolomite is generally present in veins , voids and pore spaces . Quartz is main detrital followed by feldspar . The extraclast include ...
Page 83
... dolomite , ferroan calcite , ferroan dolomite , quartz and feldspar . Dolomite is dominant in dolomicrite and dolosparite microfacies . The extradolomicrite ( limestone conglomerate ) contains subrounded to rounded clasts of biomicrite ...
... dolomite , ferroan calcite , ferroan dolomite , quartz and feldspar . Dolomite is dominant in dolomicrite and dolosparite microfacies . The extradolomicrite ( limestone conglomerate ) contains subrounded to rounded clasts of biomicrite ...
Page 85
... Dolomite , 4 = Ferroan dolomite , 5 = Quartz , 6 = Feldspar . , 7 = Others ( clay etc. ) , + + = Abundant , = Present , - = Absent . Table 6. Microfacies , faunal distribution and mineralogy based on. Sample No. Micro facies 11 ...
... Dolomite , 4 = Ferroan dolomite , 5 = Quartz , 6 = Feldspar . , 7 = Others ( clay etc. ) , + + = Abundant , = Present , - = Absent . Table 6. Microfacies , faunal distribution and mineralogy based on. Sample No. Micro facies 11 ...
Contents
CHOUBEY Kewal K Sharma D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
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02:53 IST MAGNITUDE Accel cm/sē Agglomeratic Slate Amritpur axial plane Bafliaz Formation basin biotite Budhal Burtsa Formation calcite chert clasts conglomerate Cretaceous deformation Dehra Dun deposits dolomite Dum Gali Quartzite facies fault plane feldspar folds foliation fossils Garhwal Geol gneiss grained granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology India Infrakrol Institute of Himalayan inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation Maastrichtian Mandi metamorphic Nappe Nilkanth Panjal thrust Panjal Volcanic Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone Sarkanth schist sector sedimentary sediments sequence shale Sharma shear Shergol Singh SiO2 slide slip slope soil strain Stratigraphy structures Surv Suture Zone Syncline tectonic Tethyan Thakur thick Thinly bedded Uhl valley Unconformity upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Ypresian Zanskar