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North Tibetan Plateau as an analogue for Martian environments
Session 9 - Space Exploration 4The surface of Mars preserves a variety of geomorphological structures formed by episodic hydrodynamic processes. The transition stage between the wetter and warmer early Mars and the hyper-arid environment that is today may have been characterized by strong chemical weathering by the long-term water rock interactions and the deposition of various salts. However, understanding the planetary images and geomorphology, dynamic evolution and chemical ...postprin