Results 11 to 20 of about 4,789 (265)
The Himalaya‐Karakoram‐Tibet (HKT) orogen provides an unrivaled opportunity to study the dynamic linkages between deep and surface processes during collisional orogenesis.
Ian W. Hillenbrand, Victor E. Guevara
doaj +2 more sources
Radiogenic Heating as the Thermal Driver of Himalayan Crustal Heating During Prolonged Thickening
The thermal evolution of the crust during continental collision evolves from cold to hot with time, which impacts crustal reworking and differentiation.
Shuaiqi Liu +4 more
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Orogenic Segmentation and Its Role in Himalayan Mountain Building [PDF]
The continental collision process has made a large contribution to continental growth and reconfiguration of cratons throughout Earth history. Many of the mountain belts present today are the product of continental collision such as the Appalachians, the Alps, the Cordillera, the Himalaya, the Zagros, and the Papuan Fold and Thrust Belt.
Mary Hubbard +7 more
openaire +2 more sources
Lithospheric structures of the eastern Himalayas as revealed by receiver function analysis
Although the Himalayan-Tibetan orogen is a result of compressional tectonics, the orogen also hosts active rifts accommodating east-west extension orthogonal to the north-south India-Asia convergence.
Bo Xiang +15 more
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The ca 2.0 Ga Volgo-Don fold-and-thrust belt, about 500 km in width and at least 600 km in length, covering an area of about 300000 square kilometers intervenes between the Archean Sarmatian and Volgo-Uralian proto-cratonic blocks of the East European ...
A. A. Shchipansky, T. N. Kheraskova
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Leucogranite Records Multiple Collisional Orogenies
The geological evolution of orogens is the sum of events related to both their cycle of generation as well as features inherited from their basement units.
Li Liu +9 more
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Quaternary glaciation of the Himalayan–Tibetan orogen [PDF]
AbstractGlacial geological evidence from throughout the Himalayan–Tibetan orogen is examined to determine the timing and extent of late Quaternary glaciation in this region and its relation to similar changes on a global scale. The evidence summarised here supports the existence of expanded ice caps and extensive valley glacier systems throughout the ...
Owen, L. A. +3 more
openaire +1 more source
The 1714 Bhutan earthquake was one of the largest in the Himalaya in the last millennium. We show that the surface rupture caused by this earthquake extended further to the east than previously known, it was at least 175 km long, with slip exceeding 11 m
Yuqiu Zhao +9 more
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The Bengal Basin preserves the erosional signals of coupled tectonic‐climatic change during late Cenozoic development of the Himalayan orogen, yet regional correlation and interpretation of these signals remains incomplete.
Paul M. Betka +9 more
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The occurrence of ultrahigh-pressure (UHP) and high-pressure (HP) rocks in the Himalayan orogen has been conventionally attributed to the different subduction dip angles along the strike.
Si Chen +6 more
doaj +1 more source

