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1786 Kangding-Luding earthquake : ウィキペディア英語版 | 1786 Kangding-Luding earthquake
The 1786 Kangding-Luding earthquake occurred on 1 June. It had an estimated magnitude of about 7.75 and a maximum perceived intensity of X (''Intense'') on the Mercalli intensity scale. 435 people were killed in the earthquake and a further 100,000 died following the collapse of a landslide dam across the Dadu river, triggered by an aftershock ten days later. ==Tectonic setting== Sichuan lies within the complex zone of deformation associated with the continuing collision between the India Plate and the Eurasian Plate. The thickened crust of the Tibetan plateau is spreading to the east causing the southward motion of the Sichuan-Yunnan block. The eastern side of this block is bounded by the Xianshuihe fault system, a major left lateral strike-slip fault zone. Movement on this fault zone has been responsible for many major damaging earthquakes, such as the 1981 Dawu earthquake.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「1786 Kangding-Luding earthquake」の詳細全文を読む
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