Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 251
To the east , the Pari Mountain Formation is also well exposed between Paling
and Singing in the Siang valley and in the upper reaches of the Yamne valley
where it forms high snow clad peaks . Interbands of the quartzite and biotite
schist ...
To the east , the Pari Mountain Formation is also well exposed between Paling
and Singing in the Siang valley and in the upper reaches of the Yamne valley
where it forms high snow clad peaks . Interbands of the quartzite and biotite
schist ...
Page 278
"Silurian beds are found at Trakse near Lossar in the upper Spiti on the road to
Kunzum La (32°24'N : 77°42 ' E) where they are considerably crushed and
faulted, but in other respects similar to the type series at Muth (Hayden 1904)".
"Silurian beds are found at Trakse near Lossar in the upper Spiti on the road to
Kunzum La (32°24'N : 77°42 ' E) where they are considerably crushed and
faulted, but in other respects similar to the type series at Muth (Hayden 1904)".
Page 279
of Muth and thicker ( up to 110 m ) at other localities in its vicinity , represents
upper middle Devonian or upper Devonian age . With reference to Table 1 it may
be stated that the Muth Quartzite constitutes a conformable bridge between two ...
of Muth and thicker ( up to 110 m ) at other localities in its vicinity , represents
upper middle Devonian or upper Devonian age . With reference to Table 1 it may
be stated that the Muth Quartzite constitutes a conformable bridge between two ...
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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