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龙门山断层是中国西南部龙门山的一个逆冲断层，位于青藏高原东缘，四川盆地西缘。自西向东由龙门山后山断裂、龙门山主中央断裂、龙门山主边界断裂三条平行的断裂带组成，东北-西南走向，长约500公里，宽达70公里，是地震多发区。
, The Longmenshan Fault (Chinese: 龙门山断层) is … The Longmenshan Fault (Chinese: 龙门山断层) is a thrust fault which runs along the base of the Longmen Mountains in Sichuan province in southwestern China. The strike of the fault plane is approximately NE.Motion on this fault is responsible for the uplift of the mountains relative to the lowlands of the Sichuan Basin to the east. Representing the eastern boundary of the Qinghai-Tibet Plateau, it is a border formation between the Bayan Kola block in the Plateau and the South China block in the Eurasian Plate. The 2008 Wenchuan, 2013 Lushan and 2022 Ya'an earthquakes occurred along this fault. A study by the China Earthquake Administration (CEA) states: "The late-Cenozoic deformations in this fault (that caused the 2008 Wenchuan earthquake) are concentrated in the Guanxian-Jiangyou fracture (hill-front fracture), Yingxiu-Beichuan fracture (mid-fracture), Wenchuan-Mao County fracture (hill-back fracture), and their related folds. The recent Ms 8.0 earthquake occurred on the Yingxiu-Beichuan fracture, as a result of Longmenshan thrust pushing southeastward combined with clockwise shears. Since Holocene (10,000), Yingxiu-Beichuan fracture has had evident activities. Its long-term geological slip rate is slower than 1 mm per year. GPS observations confirm the current structural deformation of the Longmenshan formation to be characterized by thrust and right-handed shears, but with a low deformation rate. Therefore, Longmenshan formation and its internal fractures constitute a special type that has low earthquake frequences but the potential to cause super strong earthquakes."ential to cause super strong earthquakes."
, 龍門山断層（りゅうもんさんだんそう、ロンメンシャンだんそう、簡体字: 龙门山断层、拼音: Lóngmén Shān Duàncéng）は、中国・四川省北部にある龍門山脈の下を走る断層である。長さ約500km、幅70kmにわたって伸びている。 地震多発地域である、2008年5月12日の四川大地震（汶川地震）や、2013年4月20日の四川地震（雅安地震）の震源はこの断層に位置している。
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龙门山断层是中国西南部龙门山的一个逆冲断层，位于青藏高原东缘，四川盆地西缘。自西向东由龙门山后山断裂、龙门山主中央断裂、龙门山主边界断裂三条平行的断裂带组成，东北-西南走向，长约500公里，宽达70公里，是地震多发区。
, The Longmenshan Fault (Chinese: 龙门山断层) is … The Longmenshan Fault (Chinese: 龙门山断层) is a thrust fault which runs along the base of the Longmen Mountains in Sichuan province in southwestern China. The strike of the fault plane is approximately NE.Motion on this fault is responsible for the uplift of the mountains relative to the lowlands of the Sichuan Basin to the east. Representing the eastern boundary of the Qinghai-Tibet Plateau, it is a border formation between the Bayan Kola block in the Plateau and the South China block in the Eurasian Plate. The 2008 Wenchuan, 2013 Lushan and 2022 Ya'an earthquakes occurred along this fault.'an earthquakes occurred along this fault.
, 龍門山断層（りゅうもんさんだんそう、ロンメンシャンだんそう、簡体字: 龙门山断层、拼音: Lóngmén Shān Duàncéng）は、中国・四川省北部にある龍門山脈の下を走る断層である。長さ約500km、幅70kmにわたって伸びている。 地震多発地域である、2008年5月12日の四川大地震（汶川地震）や、2013年4月20日の四川地震（雅安地震）の震源はこの断層に位置している。
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Longmenshan Fault
, 龙门山断层
, 龍門山断層
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