Shortening Structures in Eastern and Northwestern Himalayan Rocks |
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Page 11
... Darjeeling - Sikkim Himalaya ( Fig . 6 ) . These comprise of ( 1 ) the Precambrian high grade crystalline rocks of the Darjeeling Group and the Paro and / or Chungtang Group together with the Late Palaeozoic to Triassic Lingtse gneiss ...
... Darjeeling - Sikkim Himalaya ( Fig . 6 ) . These comprise of ( 1 ) the Precambrian high grade crystalline rocks of the Darjeeling Group and the Paro and / or Chungtang Group together with the Late Palaeozoic to Triassic Lingtse gneiss ...
Page 12
... gneiss , and foliated gneiss . Garnet is a very dominant mineral in the Paro rocks which are further exposed in the South along the boundary of the Half - Klippen of Darjeeling and Kalimpong ranges . The Darjeeling gneiss and the Paro rocks ...
... gneiss , and foliated gneiss . Garnet is a very dominant mineral in the Paro rocks which are further exposed in the South along the boundary of the Half - Klippen of Darjeeling and Kalimpong ranges . The Darjeeling gneiss and the Paro rocks ...
Page 23
... Darjeeling gneiss with a half wave - length of 25 km ) . The small - scale deformations around B4 axes also came into existence . Such a multiple deformation is documented well in the Darjeeling gneiss ( Fig . 14 ) . Fig . 14 : NNE F4 ...
... Darjeeling gneiss with a half wave - length of 25 km ) . The small - scale deformations around B4 axes also came into existence . Such a multiple deformation is documented well in the Darjeeling gneiss ( Fig . 14 ) . Fig . 14 : NNE F4 ...
Contents
INTRODUCTION | 1 |
DARJEELINGSIKKIM REGION 824 | 8 |
KUMAUNGARHWAL REGION 2539 | 25 |
Copyright | |
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Common terms and phrases
Acharyya and Ray Alaknanda Almora and/or augen gneiss autochthonous axial planes B1 and B2 B2 structures B3 and B4 Badrinath bedded Berinag Berinag Pratapnagar Buxa Central Crystalline Chail Chakrata Chandpur Chandpur-Krol Nappe cleavage planes Damuda Darjeeling Darjeeling gneiss Darjeeling-Sikkim deformation Dehra Dun Deoban Deoprayag developed exposed F1 and F2 F4 folds fold type Gansser gneiss Gondwana granite half-klippe Hercynian Himalaya Himalayan geology Himalayan rocks Joshimath Jutogh Klippe km Southwest km-stone Krol Nappe Kumaun L1 and L2 large-scale Lesser Himalaya lineations L3 Lingtse gneiss Main Central Thrust major structures metamorphism mica schist migmatites Mukhem Munsiari Nainital Nappe NNE striking NorthEast occur orogenic Palaeozoic Parautochthon Paro Paro Group phyllite phyllonites plunge Precambrian puckers quartzites Raina Ramgarh Rampur Rangit Reyang road slope S₁ S3 cleavage schists Schwan Sikkim Simla Siwalik slates southeastern Himachal SSW vergence synformal T3 planes tectonic Tertiary thrust planes Tista Half-Window transversal trend Vaikrita Valdiya vergence WNW-ESE zone