Shortening Structures in Eastern and Northwestern Himalayan Rocks |
From inside the book
Results 1-3 of 18
Page 1
... major structures . The NNE striking F1 and F2 fabrics occur on small scale . The D1 and D2 events of deformation give an idea about the pre - Himalayan ( Pre- cambrian and / or Palaeozoic ) orogenies . The D3 deformation indicated by ...
... major structures . The NNE striking F1 and F2 fabrics occur on small scale . The D1 and D2 events of deformation give an idea about the pre - Himalayan ( Pre- cambrian and / or Palaeozoic ) orogenies . The D3 deformation indicated by ...
Page 19
... structures are parallel to the major structures with regard to their form and kinematics , they can be considered as " key structures " , allowing conclusions from small- to the large - scale struc- tures . It means that in the present ...
... structures are parallel to the major structures with regard to their form and kinematics , they can be considered as " key structures " , allowing conclusions from small- to the large - scale struc- tures . It means that in the present ...
Page 52
... structures belong to another episode . The F1 and L1 structures developed in competent rocks ( e.g. quartzites and gneisses ) while F4 and L4 structures ... major structures . ( c ) Age sequence of shortening structures : The 52 W. SCHWAN.
... structures belong to another episode . The F1 and L1 structures developed in competent rocks ( e.g. quartzites and gneisses ) while F4 and L4 structures ... major structures . ( c ) Age sequence of shortening structures : The 52 W. SCHWAN.
Contents
INTRODUCTION | 1 |
DARJEELINGSIKKIM REGION 824 | 8 |
KUMAUNGARHWAL REGION 2539 | 25 |
Copyright | |
3 other sections not shown
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