Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 42
THARUMSA MEMBER This unit ( ~ 460 m thick ) consists mainly of grey ,
medium to coarse grained sandstone ( sometimes gritty ) and grey to black
carbonaceous shale in the lower part ; fine to medium grained grey sandstone
and shale ...
THARUMSA MEMBER This unit ( ~ 460 m thick ) consists mainly of grey ,
medium to coarse grained sandstone ( sometimes gritty ) and grey to black
carbonaceous shale in the lower part ; fine to medium grained grey sandstone
and shale ...
Page 199
10 ) ( Kuhle 1988c ) . It was a transfluence pass , with a minimum ice thickness of
250 - 400 m ( Fig . ... These moraines and erratics are evidence of a Hunza
Glacier more than 1000 m thick and an ice surface at 3500 m asl . As erratics
indicate ...
10 ) ( Kuhle 1988c ) . It was a transfluence pass , with a minimum ice thickness of
250 - 400 m ( Fig . ... These moraines and erratics are evidence of a Hunza
Glacier more than 1000 m thick and an ice surface at 3500 m asl . As erratics
indicate ...
Page 202
This ice stream was three times thicker than the 500 m supposed by Kamp ( 1999
) . ... This means that an over 1000 m thick LGM ice stream network existed in this
area , which was connected to the Karakoram ice stream network across the ...
This ice stream was three times thicker than the 500 m supposed by Kamp ( 1999
) . ... This means that an over 1000 m thick LGM ice stream network existed in this
area , which was connected to the Karakoram ice stream network across 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