首页> 外文期刊>Open Journal of Geology >Re-Estimation of a Plausible Model of the Earthquake Fault as the Source of the 1771 Great Meiwa Tsunami Based on the Assessment of the Run-Up Height by Okinawa Prefecture, Japan
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Re-Estimation of a Plausible Model of the Earthquake Fault as the Source of the 1771 Great Meiwa Tsunami Based on the Assessment of the Run-Up Height by Okinawa Prefecture, Japan

机译:重新估算地震断层的合理模型,作为1771年伟大的Meiwa海啸来源,基于日本冲绳县的奔跑高度评估

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Plausible parameters of the earthquake fault which caused the 1771 Great Meiwa Tsunami were re-estimated by comparing the result of the tsunami run-up height by the numerical simulation by Okinawa Prefectural Government and those by 1) run-up height derived from previous field works, and 2) a historical record describing the run-up height in Miyako District. The re-estimation shows that the length of the fault off Miyako and Yaeyama districts is 300 km or more. However, the slip of the fault is 20 m off Yaeyama and 8 - 14 m off Miyako.
机译:通过通过冲绳县政府的数值模拟和1)从以前的实地运作,通过比较海啸射程高度的结果,通过比较了从先前的实地工作的数量模拟来重新估算了造成1771年伟大的Meiwa海啸的地震断层的似估计。 2)一个描述Miyako区延伸高度的历史记录。重新估计表明,Miyako和Yaeyama区的断层长度为300公里或以上。然而,yaeyama的故障滑动是yaeyama和8 - 14米的近距离。

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