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The Kunlun fault is a strike-slip fault to the north side of Tibet. Slippage along the 1,500 kilometres (930 mi) long fault has occurred at a constant rate for the last 40,000 years. This has resulted in a cumulative offset of more than 400 metres (1,300 ft). The fault is seismically active, most recently causing the magnitude 7.8 2001 Kunlun earthquake. It forms the northeastern boundary of the elongate wedge of the Tibetan Plateau known as the Bayan Har block.

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  • Sesar Kunlun (in)
  • Kunlun Fault (en)
  • Куньлуньский разлом (ru)
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  • The Kunlun fault is a strike-slip fault to the north side of Tibet. Slippage along the 1,500 kilometres (930 mi) long fault has occurred at a constant rate for the last 40,000 years. This has resulted in a cumulative offset of more than 400 metres (1,300 ft). The fault is seismically active, most recently causing the magnitude 7.8 2001 Kunlun earthquake. It forms the northeastern boundary of the elongate wedge of the Tibetan Plateau known as the Bayan Har block. (en)
  • Sesar Kunlun adalah sesar mendatar yang terjadi di bagian utara Tibet. Patahan sepanjang 1.500 km pada tingkat yang konstan telah berlangsung selama 40.000 tahun terakhir, dan menghasilkan offset kumulatif lebih dari 400 meter. Secara seismik, sesar Kunlun termasuk kategori aktif, dan menyebabkan gempa bumi Kunlun 2001 dengan magnitudo 7,8 Mw. (in)
  • Куньлуньский разлом — разлом со смещением по простиранию на северной стороне Тибета. Сдвиг вдоль разлома длиной 1 500 километров происходил с постоянной скоростью в течение последних 40 000 лет. Это привело к суммарному смещению более чем на 400 метров. Разлом сейсмически активен, последний раз он вызвал Куньлуньское землетрясение 2001 года магнитудой 7,8. Куньлуньский разлом образует северо-восточную границу вытянутого клина Тибетского нагорья, известного как Баян-Хар. (ru)
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  • The Kunlun fault is a strike-slip fault to the north side of Tibet. Slippage along the 1,500 kilometres (930 mi) long fault has occurred at a constant rate for the last 40,000 years. This has resulted in a cumulative offset of more than 400 metres (1,300 ft). The fault is seismically active, most recently causing the magnitude 7.8 2001 Kunlun earthquake. It forms the northeastern boundary of the elongate wedge of the Tibetan Plateau known as the Bayan Har block. (en)
  • Sesar Kunlun adalah sesar mendatar yang terjadi di bagian utara Tibet. Patahan sepanjang 1.500 km pada tingkat yang konstan telah berlangsung selama 40.000 tahun terakhir, dan menghasilkan offset kumulatif lebih dari 400 meter. Secara seismik, sesar Kunlun termasuk kategori aktif, dan menyebabkan gempa bumi Kunlun 2001 dengan magnitudo 7,8 Mw. (in)
  • Куньлуньский разлом — разлом со смещением по простиранию на северной стороне Тибета. Сдвиг вдоль разлома длиной 1 500 километров происходил с постоянной скоростью в течение последних 40 000 лет. Это привело к суммарному смещению более чем на 400 метров. Разлом сейсмически активен, последний раз он вызвал Куньлуньское землетрясение 2001 года магнитудой 7,8. Куньлуньский разлом образует северо-восточную границу вытянутого клина Тибетского нагорья, известного как Баян-Хар. (ru)
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