1997 Manyi earthquake
http://dbpedia.org/resource/1997_Manyi_earthquake an entity of type: Thing
The 1997 Manyi earthquake (Chinese: 玛尼地震) occurred on November 8 at 10:02 UTC. The epicenter was in Nagqu Prefecture in northern Tibet, China. The focal mechanism indicates a left-lateral strike-slip movement. This earthquake had a surface rupture of 17 km (11 mi) long with up to 7 m (23 ft) of left-lateral slip along the Manyi fault, a westward continuation of the Kunlun fault, offset about 100 km (62 mi) to the south. Normally, the continental crust is about 35 km (22 mi) thick, but it reaches 70 km (43 mi) thick under the Tibetan Plateau. This earthquake ruptured up to 20 km (12 mi) of the top part of the local continental crust.
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Jordbävningen i Manyi 1997 inträffade den 8 november 1997 klockan 10:02 UTC. Epicentrum fanns i prefekturen Nagchu (那曲地區) i norra Tibet, Kina. Fokusmekanismen indikerar en rörelse i hissriktning. Sprickan i ytan blev 170 kilometer lång vid Manyiförkastningen, en västlig fortsättning , cirka 100 kilometer söderut. Normalt är kontinentalplattan omkring 35 kilometer tjock, men når 70 kilometer under Tibitanska platån. Jordbävningen spräckte upp till 20 kilometer av kontinentalplattans topp.
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1997 Manyi earthquake
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Jordbävningen i Manyi 1997
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The 1997 Manyi earthquake (Chinese: 玛尼地震) occurred on November 8 at 10:02 UTC. The epicenter was in Nagqu Prefecture in northern Tibet, China. The focal mechanism indicates a left-lateral strike-slip movement. This earthquake had a surface rupture of 17 km (11 mi) long with up to 7 m (23 ft) of left-lateral slip along the Manyi fault, a westward continuation of the Kunlun fault, offset about 100 km (62 mi) to the south. Normally, the continental crust is about 35 km (22 mi) thick, but it reaches 70 km (43 mi) thick under the Tibetan Plateau. This earthquake ruptured up to 20 km (12 mi) of the top part of the local continental crust.
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Jordbävningen i Manyi 1997 inträffade den 8 november 1997 klockan 10:02 UTC. Epicentrum fanns i prefekturen Nagchu (那曲地區) i norra Tibet, Kina. Fokusmekanismen indikerar en rörelse i hissriktning. Sprickan i ytan blev 170 kilometer lång vid Manyiförkastningen, en västlig fortsättning , cirka 100 kilometer söderut. Normalt är kontinentalplattan omkring 35 kilometer tjock, men når 70 kilometer under Tibitanska platån. Jordbävningen spräckte upp till 20 kilometer av kontinentalplattans topp.
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