Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 334
DISCUSSION Comparison between the eastern Himalayan syntaxis and the
central to eastern Himalaya A comparison of the eastern Himalayan syntaxis with
the central to eastern Himalayas , which are well - known Himalayan areas ,
might ...
DISCUSSION Comparison between the eastern Himalayan syntaxis and the
central to eastern Himalaya A comparison of the eastern Himalayan syntaxis with
the central to eastern Himalayas , which are well - known Himalayan areas ,
might ...
Page 335
These observations clearly suggest that although the eastern Himalayan syntaxis
occupies a special tectonic position within the Himalaya , it shares numerous
similarities with the central to eastern Himalayas . The lithostratigraphic units and
...
These observations clearly suggest that although the eastern Himalayan syntaxis
occupies a special tectonic position within the Himalaya , it shares numerous
similarities with the central to eastern Himalayas . The lithostratigraphic units and
...
Page 337
Gansser , A . 1983 Geology of the Bhutan Himalaya . Birkhauser Verlag Basel
181p . Goscombe , B . , Hand , M . 2000 Contrasting P - T paths in the eastern
Himalaya , Nepal : Inverted isograds in a paired metamorphic mountain belt .
Gansser , A . 1983 Geology of the Bhutan Himalaya . Birkhauser Verlag Basel
181p . Goscombe , B . , Hand , M . 2000 Contrasting P - T paths in the eastern
Himalaya , Nepal : Inverted isograds in a paired metamorphic mountain belt .
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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