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Page 192
Its radiocarbon age and equilibrium line depression bring it into line with other
moraines , such as the terminal moraine at ... Ice marginal positions and the
extent of outlet glaciers flowing down from South Tibet are based on riverside
moraine ...
Its radiocarbon age and equilibrium line depression bring it into line with other
moraines , such as the terminal moraine at ... Ice marginal positions and the
extent of outlet glaciers flowing down from South Tibet are based on riverside
moraine ...
Page 201
... temperature of 3 . 1°C during the period 1957 - 1980 . The lowest moraines of
the LGM are at 2000 - 1900 m asl ( Kuhle 1994 ) . Tens of kilometres long , these
chains of medial moraines extend the transverse valleys of the Kuen - Lun ...
... temperature of 3 . 1°C during the period 1957 - 1980 . The lowest moraines of
the LGM are at 2000 - 1900 m asl ( Kuhle 1994 ) . Tens of kilometres long , these
chains of medial moraines extend the transverse valleys of the Kuen - Lun ...
Page 203
In the north / east facing Oytag Valley of the King Ata Tagh Mountains ( Fig . 2 No
. 37 ) , which rise to 6800 or 6634 m asl ( Kara - Bak - Tor Peak ) , the lowest LGM
ice margin , confirmed by till and end moraines , extended down to 1850 m asl ...
In the north / east facing Oytag Valley of the King Ata Tagh Mountains ( Fig . 2 No
. 37 ) , which rise to 6800 or 6634 m asl ( Kara - Bak - Tor Peak ) , the lowest LGM
ice margin , confirmed by till and end moraines , extended down to 1850 m asl ...
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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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Common terms and phrases
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
Bibliographic information
| Title | Himalaya: Geological Aspects, Volume 4 Volume 15 of Current trends in geology Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 4 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Publishing House, 2005 |
| Original from | the University of Michigan |
| Digitized | 19 Feb 2010 |
| ISBN | 818930402X, 9788189304027 |
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