Multilevel mechanisms driving intraplate volcanism in Central Mongolia revealed by adjoint waveform tomography of receiver function and ambient noise data
The genesis of the Cenozoic intraplate volcanism in Central Mongolia, characterized by sustained and low-volume eruptions remains debated due to the lack of a comprehensive model to interpret the Cenozoic volcanic activities. Here, we introduce a high-resolution 3D velocity model of the Hangay Dome,...
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Main Authors: | , , , , , , , |
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格式: | Article |
語言: | English |
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2025
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在線閱讀: | https://hdl.handle.net/10356/182602 |
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