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The article discusses the LUSI mud volcano in Indonesia, which erupted on May 29, 2006, due to the release of overpressure from deep sediments, resulting in significant mud and gas flow that has displaced thousands of residents. The eruption dynamics were influenced by nearby seismic activity and a high temperature gradient from a magmatic complex, leading to a quasi-hydrothermal system. The study provides insights into the geological processes and eruption mechanisms, highlighting the unique opportunity to

Author

shope0384

Language

EN