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Poster Programme TS4.5

TS4.5

Geodynamics of collisional type orogenic belts and plateaus and its response to climate and erosional process - Himalaya, Pamir, Central Asia & Tibet
Convener: R. Thiede  | Co-Conveners: M. Fuchs , M. Allen 
Oral Programme
 / Mon, 23 Apr, 10:30–12:00  / 13:30–17:00  / Room 20
Poster Programme
 / Attendance Mon, 23 Apr, 17:30–19:00  / Hall A

Attendance Time: Monday, 23 April 2012, 17:30–19:00
Hall A
Chairperson: Thiede, Mukherjee, Fuchs, Jolivet, Allen
A394
EGU2012-10559
Foreland out-of Sequence thrusting and rapid Pleistocene exhumation of Higher Himalayan crustal rocks in the Western Arunachal Himalaya
G. Mathew et al.

A395
EGU2012-8172
Structural Framework of the Sub-Himalaya and its tectonic evolution along Kameng river section: Arunachal Pradesh, India
T. Goswami et al.

A396
EGU2012-4548
Large Spatial and Temporal Variations in Himalayan Denudation
R. Thiede and T. Ehlers

A397
EGU2012-5232
Strong Coupled and Segmented Nature of the Himalaya and the Adjoining Gangetic Foreland Basin
B. Parkash et al.

A398
EGU2012-5383
Influence of active fault on the evolution of landscape and drainage: Evidence from lateral propagation of a branching out fault along Himalayan front and deflection of Dabka River, Kumaun Himalayas
A. Shah et al.

A399
EGU2012-10972
Postglacial denudation outpaced by long-term exhumation, Ladakh and Zanskar, India
H. Munack et al.

A400
EGU2012-11424
Himalayan orogeny and palaeovegetational changes: a relook into the factors controlling global expansion of C4 grasslands.
S. Singh et al.

A401
EGU2012-5294
Active faults in the Kashmir Valley
A. Shah

A402
EGU2012-5684
Trapezoid-shaped mineral grains in micro-scale from the Higher Himalayan Shear Zone, Sutlej section, Indian Himalaya: their morphometry and tectonic implications
S Mukherjee and P Nasipuri

A403
EGU2012-3582
Prograde fluid in Tso Morari UHP rocks, Ladakh India
B. Mukherjee and S. Mukherjee

A405
EGU2012-3597
Microstructures and kinematic vorticity analysis from the mylonites along the Karakoram Shear Zone, Pangong Mountains, Karakoram
P. Roy

A406
EGU2012-5707
Viscous dissipations in simple shear zones- analytical models and a Himalayan example
P. Nasipuri and S Mukherjee

A407
EGU2012-3601
Structural geology of the Bhagirathi section of the Higher Himalayan Shear Zone with special reference to back-thrusting
P. Roy and S. Mukherjee

A409
EGU2012-3853
Rates and kinematics of deformations along the eastern Qilian Shan Mountain, NE Tibetan Plateau, constraint by deformed fluvial terraces
X. Hu et al.

A410
EGU2012-10971
Extensional step-over between the Zhongdian and Red River faults: kinematics of the Daju normal fault constrained by cosmogenic dating of the Yangtze terraces (Yulong Shan, Yunnan)
J. van der Woerd et al.

A411
EGU2012-4095
Opposite block rotation in westernmost Yunnan at present and during the last 5 Ma?
D. Kornfeld et al.

A413
EGU2012-8053
Tectonically controlled relief evolution in the Northern Tien Shan and Junggar Alatau from the Eocene to the Present
N. Seib et al.

A415
EGU2012-5452
Evolution of the Qimantagh magmatic arcs: constraints from U-Pb zircon ages and implications for subduction of Proto- and Paleo-Tethyan Oceans
W. Li et al.

A417
EGU2012-4965
Evidence for southward subduction beneath the eastern Pamir constrained by teleseismic converted seismic waves
F. M. Schneider et al.

A418
EGU2012-10528
Suspended sediment flux characteristics in the central Pamirs
E. Pohl and R. Gloaguen

A419
EGU2012-13283
Two-/three-dimensional thermo-mechanical modeling of Cenozoic lithospheric deformation in the Himalaya-Tibet-Pamir-Tien Shan orogen
J. Tympel and S. Sobolev

A420
EGU2012-1133
What drives the Tibetan crust to the South East Asia? Role of upper mantle density discontinuities as inferred from the continental geoid anomalies
S. Rajesh

A421
EGU2012-10343
Numerical model of continental collision: comparison between Variscan (Bohemian Massif) and modern (Himalayan) orogeny
P. Maierová et al.

A422 EGU2012-10662
Variation in Erosion Rates in Sikkim Himalaya for the past 5 Myr (withdrawn)
S. Dey and R. Thiede