Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 154
According to Kumar and Aggarwal ( 1975 ) , the Pauri phyllite forms a formation
of the Dudatoli Group and is also included in ... Near Barkot and Koteshwar the
phyllites show development of slickensides plunging in NNE and SSW direction .
According to Kumar and Aggarwal ( 1975 ) , the Pauri phyllite forms a formation
of the Dudatoli Group and is also included in ... Near Barkot and Koteshwar the
phyllites show development of slickensides plunging in NNE and SSW direction .
Page 157
The geological cross section ( Fig 2 ) from Srinagar to Margaon reveals that in
SW part of the area the quartzites are tectonically overlain by the Srinagar
phyllites . Along Srinagar - Margaon section the phyllites are missing due to
erosion and ...
The geological cross section ( Fig 2 ) from Srinagar to Margaon reveals that in
SW part of the area the quartzites are tectonically overlain by the Srinagar
phyllites . Along Srinagar - Margaon section the phyllites are missing due to
erosion and ...
Page 161
The lithology of Chail nappe - 1 is of phyllites while Chail Nappe - 2 consists of
quartzites , slates and limestone of the Garhwal Group . Chail Nappe - 1 The
Chandpur / Pauri Phyllites constituting the nappe are delineated at the base by
the ...
The lithology of Chail nappe - 1 is of phyllites while Chail Nappe - 2 consists of
quartzites , slates and limestone of the Garhwal Group . Chail Nappe - 1 The
Chandpur / Pauri Phyllites constituting the nappe are delineated at the base by
the ...
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Contents
Evidence | 1 |
Tectonomagmatic Evolutionary Model of the KuluRampur | 47 |
Tectonic and Geochemical Signifcance of Black Shale | 65 |
Copyright | |
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active Alaknanda Arunachal associated bands basin beds belt biotite Central characterized concentration Crystalline deformation Delhi deposits developed direction drainage Early east eastern elements et al evidence exposed extending fault field Figure folds Formation fractures further Garhwal Geol Geological Glacial glacier gneisses grains granite granitoids Group Himalaya India indicate Indus Kuhle Ladakh Late length Lesser limestone lineaments Lower Main major margin metamorphic moraines mountain nature ND ND normal northern Nummulitic observed occur Pakistan parallel pattern phyllites places plane plate Pleistocene Pradesh present quartzite range region represented resulted river rocks Saklani samples schist sediments sequence shale Siang districts side similar Siyom slide slope southern streams structural studies suggest surface Suture Table tectonic thick thrust Tibet trend unit upper valley values Volcanics western zone