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The 2008 Sichuan earthquake occurred along a convergent boundary, specifically at the intersection of the Indian Plate and the Eurasian Plate. This tectonic interaction involves the subduction of the Indian Plate beneath the Eurasian Plate, leading to significant stress accumulation and eventual release, which caused the earthquake. The region is known for its complex geology and seismic activity due to these tectonic processes.

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1w ago

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