Geology and Geodynamic Evolution of the Himalayan Collision Zone, Volume 18, Parts 1-2Kewal K. Sharma |
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Page 203
... tectonites are of chrome diopside . Several mineral analyses are listed in Table 1. The orthopyroxene crystal grains of harzburgite in the Langqen Zangbo ophiolite belt and the western segment of Yarlung Zangbo ophiolite belt always ...
... tectonites are of chrome diopside . Several mineral analyses are listed in Table 1. The orthopyroxene crystal grains of harzburgite in the Langqen Zangbo ophiolite belt and the western segment of Yarlung Zangbo ophiolite belt always ...
Page 204
... tectonites in the Langen Zangbo belt as it is located on the concave side of the north margin of India landmass . While the eastern segment of Yarlung Zangbo ophiolite belt was intensely squeezed during the later phase of collision ...
... tectonites in the Langen Zangbo belt as it is located on the concave side of the north margin of India landmass . While the eastern segment of Yarlung Zangbo ophiolite belt was intensely squeezed during the later phase of collision ...
Page 209
... tectonites are similar to that of Alpine ultramafic rocks in other areas of the world . The unaltered dunite in Dagzhuka massif contains the highest content of MgO ( Table 2 , No. 1 ) . The con- tents of iron and chromium in the ...
... tectonites are similar to that of Alpine ultramafic rocks in other areas of the world . The unaltered dunite in Dagzhuka massif contains the highest content of MgO ( Table 2 , No. 1 ) . The con- tents of iron and chromium in the ...
Contents
LHASA SECTOR | 193 |
Regional framework and tectonics of the Yarlung | 221 |
Sedimentology of trencharc sediments and | 237 |
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active Andaman anomaly appears associated basalt basin block Central chert close collision complex components Congdu continental Cretaceous crustal cumulate deposits depth Early Earth earthquake eastern elements Eocene et al evolution facies fault field Formation formed fossils Geol Geology granite gravity Group Hills Himalaya India indicate Indus island arc Kashmir Kohistan Ladakh Late lava Lhasa limestone located Lohit lower magmatic major mantle margin massif melange metamorphism Mishmi Moho Molnar mountains movement Naga nature northern obducted observed occur oceanic ophiolite belt plane plate plateau Pleistocene present Qinghai range region reported represent rocks samples sector sedimentary sediments seismicity sequence Shan Sharma shown solutions southern structure studies subduction suggest Suture suture zone Table tectonic Tethys thick thrust Tibet trench trend turbidite ultramafic unit upper volcanic western Xigaze Xizang Yarlung Zangbo zone