Shortening Structures in Eastern and Northwestern Himalayan Rocks |
From inside the book
Results 1-3 of 10
Page 8
... large - scale translation from the Great to the Lesser Himalaya . Very remarkable is the phenomenon of the inverted metamorphism . This refers to the increasing metamorphic grade , observed upward from the Lesser to the Higher Himalaya ...
... large - scale translation from the Great to the Lesser Himalaya . Very remarkable is the phenomenon of the inverted metamorphism . This refers to the increasing metamorphic grade , observed upward from the Lesser to the Higher Himalaya ...
Page 24
... scale . At times , the F5 structures are associated with parallel steep fractures . In the Darjeeling - Sikkim ... large - scale . The B5 is developed mainly on large - scale . KUMAUN - GARHWAL REGION Tectonic Setting : The area between ...
... scale . At times , the F5 structures are associated with parallel steep fractures . In the Darjeeling - Sikkim ... large - scale . The B5 is developed mainly on large - scale . KUMAUN - GARHWAL REGION Tectonic Setting : The area between ...
Page 52
... scale only ( e . g . F1 and F2 ) or on large - scale ( e.g. F5 ) or on both scales ( e.g. F3 and F4 ) . ( b ) Relationship of large and small - scale structures : The compressional forces formed large - scale and small - scale planar ...
... scale only ( e . g . F1 and F2 ) or on large - scale ( e.g. F5 ) or on both scales ( e.g. F3 and F4 ) . ( b ) Relationship of large and small - scale structures : The compressional forces formed large - scale and small - scale planar ...
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