Review on dating methods: Numerical dating in the quaternary geology of High Asia

@article{Kuhle2010ReviewOD,
  title={Review on dating methods: Numerical dating in the quaternary geology of High Asia},
  author={Matthias Kuhle and Sabine Kuhle},
  journal={Journal of Mountain Science},
  year={2010},
  volume={7},
  pages={105-122}
}
Over the past few years, OSL and TCN datings of glacial material from High Asia have come into fashion. To this day, however, these techniques do not permit safe calibration. The intensity of the cosmic ray flux is being modulated by the solar and terrestrial magnetic fields and their secular fluctuations in the past. So far, these variations cannot be converted into the respective local TCN production rates for High Asia. We have reason to believe that the ages that are being calculated… 
The glacial (MIS 3-2) outlet glacier of the Marsyandi Nadi-icestream-network with its Ngadi Khola tributary glacier (Manaslu- and Lamjung Himalaya): The reconstructed lowering of the Marsyandi Nadi ice stream tongue down in to the southern Himalaya Foreland
  • M. Kuhle
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Like for most parts of High Asia, researches concerning the Pleistocene landscape evolution of the Leh Basin (34°03′ N/77°38′ E) have also left contradictions. To push this topic, three up to now
Changes in the thermal and hydraulic regime within the active layer in the Qinghai-Tibet Plateau
The change trends of air temperature, precipitation and evaporation from 1999 to 2008 shows that the climate in the Qinghai-Tibet Plateau permafrost region had become warmer. The analysis of the
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Defining a basin under a critical state (or a self-organized criticality) that has the potential to initiate landslides, debris flows, and subsequent sediment disasters, is a key issue for disaster
In memoriam: Matthias Kuhle
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