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Source mechanism of the 1998 Mw 7.4 intraplate strike-slip earthquake in the West Philippine Basin revealed by Coulomb stress changes
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文摘
The source mechanism of the 1998 Mw 7.4 oceanic intraplate earthquake in the WPS was determined. The oceanic intraplate earthquakes in the WPS do not rupture along the pre-existing fracture features. The CFS produced by a large oceanic intraplate earthquake could affect its nearby subduction system.

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