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Effects of Rupture Processes in an Inverse Analysis of the Tsunami Source of the 2011 Off the Pacific Coast of Tohoku Earthquake

机译:东北太平洋2011年海啸源海啸破裂过程的破裂过程影响

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摘要

An inverse analysis of the tsunami source of the 2011 earthquake off the Pacific coast of Tohoku (Mw 9.0) was conducted on the basis of offshore sea-level observation near the source area. The effects of the rupture process on tsunami source inversion were investigated by comparing tsunami source models that assumed either infinite or finite rupture velocities.
机译:在震源区附近的海平面观测的基础上,对2011年东北太平洋沿岸海域地震(Mw 9.0)进行了海啸源反演。通过比较假定无限或有限破裂速度的海啸震源模型,研究了破裂过程对海啸震源反演的影响。

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