Geology and geodynamic evolution of the Himalayan collision zone, Volume 18, Parts 1-2 |
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Page 237
The Cretaceous olistostromes (Zongzhuo Formation) probably of Albian age
might be earlier trench-slope deposits. The trench turbidite together with slope
olistostromes may constitute the residual accretions ry prism of a trench-
subduction ...
The Cretaceous olistostromes (Zongzhuo Formation) probably of Albian age
might be earlier trench-slope deposits. The trench turbidite together with slope
olistostromes may constitute the residual accretions ry prism of a trench-
subduction ...
Page 241
suggested that both the basal and the overthrusted pillow lava slices represent
the younger oceanic crust unit on which the trench turbidites were deposited. Fig.
2. Congdu and Bainang sections southeast of Xigase, involving trench turbidite.
suggested that both the basal and the overthrusted pillow lava slices represent
the younger oceanic crust unit on which the trench turbidites were deposited. Fig.
2. Congdu and Bainang sections southeast of Xigase, involving trench turbidite.
Page 265
Figure 9b which matched the section II in Fig.2 shows that the basal serpentinite
of ophiolite was obducted northwards on the Congdu trench turbidite. There, the
thrusted contact of the ultramafics is facing to the south, while the turbidites are ...
Figure 9b which matched the section II in Fig.2 shows that the basal serpentinite
of ophiolite was obducted northwards on the Congdu trench turbidite. There, the
thrusted contact of the ultramafics is facing to the south, while the turbidites are ...
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Contents
LHASA SECTOR | 195 |
Regional framework and tectonics of the Yarlung | 221 |
Sedimentology of trencharc sediments and | 237 |
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Acharyya Andaman anomaly Assam basalt basin blueschist chert conglomerate continental Cretaceous crustal crystalline cumulate deposits dunite earthquake eastern Eocene evolution facies fault flysch Formation fossils gabbro GANSSER Geodynamic Geol Geology Geophy gravity field harzburgite high-P Himalaya Himalayan collision zone India Indian plate Indus Suture Indus-Tsangpo Suture island arc Jurassic Kashmir Klootwijk Kohistan Kumaun Ladakh Lhasa Lhasa block limestone located Lohit magmatic mantle margin massif mega-belt melange metamorphism Mishmi Moho Molnar Naga Hills Nandy Nanga Parbat northern northward NW Himalaya obducted occur oceanic crust ophiolite ophiolite melange Pakistan Palaeomagnetism pillow lava plutonic pole positions Qing-Zang plateau Qinghai-Xizang Plateau region samples sandstone schists sector sedimentary sediments seismicity sequence Shan Sharma strike-slip structure studies subduction suture zone tectonic tectonites Terrane Tertiary Tethyan Tethys tholeiitic thrust Tibet trench turbidite turbidite ultramafic upper Verma volcanic rocks Xigaze Xigaze Group Xizang Yarlung Zangbo ophiolite
Bibliographic information
| Title | Geology and geodynamic evolution of the Himalayan collision zone, Volume 18, Parts 1-2 Physics and chemistry of the earth Geology and Geodynamic Evolution of the Himalayan Collision Zone, Kewal K. Sharma |
| Editor | Kaushal Kishore Sharma |
| Publisher | Pergamon Press, 1991 |
| Original from | the University of Michigan |
| Digitized | 13 Apr 2010 |
| Length | 446 pages |
| Subjects | Geochemistry Geodynamics Geology Plate tectonics |
| Export Citation | BiBTeX EndNote RefMan |