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Yin's research was focused on studying how mountains are created and destroyed on Earth and other solar-system bodies. His work on Earth was field-based, which starts with making detailed geologic maps and ends with the construction of kinematic and mechanical models of the evolution of Earth's lithosphere. Based on analysis of satellite images and comparison against similar geologic settings from the Earth such as the western Pacific subduction system, Yin proposed a hypothesis that a primitive form of plate tectonics, expressed as local plate boundary processes involving thermal-boundary-layer recycling by impact-induced slab rollback, may have been responsible for the formation of the Tharsis rise on Mars. His proposed primitive plate tectonics differs from the modern plate tectonics on Earth, which operates over the entire planet.
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JOURNAL OF HYDROLOGY (2024): 130810
Earth and Planetary Science Letters (2024): 118743
Icaruspp.116064, (2024)
Geological Society of America Abstracts with Programsno. 1 (2023): 1-8
Geologyno. 4 (2023): 413-413
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