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・ 1983 Rose Bowl
・ 1983 Royal Artillery Barracks bombing
・ 1983 RTHK Top 10 Gold Songs Awards
・ 1983 Ryder Cup
・ 1983 Samoa National League
・ 1983 San Diego Chargers season
・ 1983 San Diego Padres season
・ 1983 San Francisco 49ers season
・ 1983 San Francisco Giants season
・ 1983 San Marino Grand Prix
・ 1983 San Miguel Beermen season
・ 1983 SANFL Grand Final
・ 1983 SANFL season
・ 1983 Scott Tournament of Hearts
・ 1983 Scottish Cup Final
1983 Sea of Japan earthquake
・ 1983 Seattle Mariners season
・ 1983 Seattle Seahawks season
・ 1983 SEC Men's Basketball Tournament
・ 1983 SEC Women's Basketball Tournament
・ 1983 Senior PGA Tour
・ 1983 Skate America
・ 1983 Skate Canada International
・ 1983 Sligo Intermediate Football Championship
・ 1983 Sligo Senior Football Championship
・ 1983 South African Grand Prix
・ 1983 South African motorcycle Grand Prix
・ 1983 South African Open (tennis)
・ 1983 South American Championships in Athletics
・ 1983 South American Junior Championships in Athletics


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1983 Sea of Japan earthquake : ウィキペディア英語版
1983 Sea of Japan earthquake

The 1983 Sea of Japan earthquake or 1983 Nihonkai-Chubu earthquake occurred on May 26, at 11:59:57 local time (02:59:59.6 UTC), It had a magnitude of 7.8 on the moment magnitude scale. It occurred in the Sea of Japan, about 100 km west of the coast of Noshiro in Akita Prefecture, Japan. Out of the 104 fatalities, all but four were killed by the resulting tsunami, which struck communities along the coast, especially Aomori and Akita Prefectures and the east coast of Noto Peninsula. Images of the tsunami hitting the fishing harbor of Wajima on Noto Peninsula was broadcast on TV. The waves exceeded in some areas. Three of the fatalities were along the east coast of South Korea (whether North Korea was affected is not known). The tsunami also hit Okushiri Island, the site of a more deadly tsunami 10 years later.
==Tectonic setting==
The northwestern side of Honshu lies on the southeastern margin of the Sea of Japan, an area of oceanic crust created by back-arc spreading from the late Oligocene to middle Miocene. The extensional tectonics associated with the spreading formed a series of N-S trending extensional faults and associated basins. Currently the area is being deformed by contractional tectonics, causing inversion of these earlier basins, forming anticlinal structures. It has been suggested that the northwestern coast of Honshu represents an incipient subduction zone,〔 but there remain significant uncertainties about the existence of the Okhotsk Plate and the nature and precise location of its boundary in the Sea of Japan, if it does exist.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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