@article{GaoZeilingerXuetal.2013,
  author    = {Gao, Mingxing and Zeilinger, Gerold and Xu, Xiwei and Wang, Qingliang and Hao, Ming},
  title     = {DEM and GIS analysis of geomorphic indices for evaluating recent uplift of the northeastern margin of the Tibetan Plateau, China},
  series = {Geomorphology : an international journal on pure and applied geomorphology},
  volume    = {190},
  journal   = {Geomorphology : an international journal on pure and applied geomorphology},
  number    = {20},
  publisher = {Elsevier},
  address   = {Amsterdam},
  issn      = {0169-555X},
  doi       = {10.1016/j.geomorph.2013.02.008},
  pages     = {61 -- 72},
  year      = {2013},
  abstract  = {The northeastern margin of the Tibetan Plateau is a tectonically active region consisting of a series of faults with bounded intermountain basins and is located in the transition zone between the Tibetan Plateau and the Loess Plateau. Active deformation that may affect the topography in this region can be quantified using geomorphic indices. Therefore, we applied geomorphic indices such as the hypsometric integral and the stream length gradient index to infer neo-tectonics in the northeastern margin of the Tibetan Plateau. Different time-scaled geodetic leveling data and river incision rates were also integrated into the investigation. The results show that the hypsometric integrals are not significantly affected by lithology but spatially correspond to the hanging walls of thrust faults. The hypsometric integrals are also positively correlated with the leveling data. Although the stream length gradient index is influenced by lithology, its most pronounced anomalies of the stream length gradient are associated with the thrust faults. Consequently, the uplift in the northeast margin of the Tibetan Plateau appeared to be concentrated along the hanging walls of the thrust faults.},
  language  = {en}
}
@article{KirbyHarkins2013,
  author    = {Kirby, Eric and Harkins, Nathan},
  title     = {Distributed deformation around the eastern tip of the Kunlun fault},
  series = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
  volume    = {102},
  journal   = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
  number    = {7},
  publisher = {SPRINGER},
  address   = {NEW YORK},
  issn      = {1437-3254},
  doi       = {10.1007/s00531-013-0872-x},
  pages     = {1759 -- 1772},
  year      = {2013},
  abstract  = {Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relatively little is known about how displacement along these structures is accommodated at fault terminations. Here, we show that a systematic decrease in left-lateral slip rates along the eastern similar to 200 km of the Kunlun fault, from > 10 mm/year to < 1 mm/year, is coincident with high topography in the Anyemaqen Shan and with a broad zone of distributed shear and clockwise vorticity within the Tibetan Plateau. Geomorphic analysis of river longitudinal profiles, coupled with inventories of cosmogenic radionuclides in fluvial sediment, reveal correlated variations in fluvial relief and erosion rate across the Anyemaqen Shan that reflect ongoing differential rock uplift across the range. Our results imply that the termination of the Kunlun fault system is accommodated by a combination of distributed crustal thickening and by clockwise rotation of the eastern fault segments.},
  language  = {en}
}