地球学报Issue(3)：391-394,4.DOI:10.3975/cagsb.2014.03.15
2014年于田Ms7.3地震野外调查--特殊的地表破裂带
Field Study of the 12 February 2014 Yutian Ms7.3 Earthquake:A Special Surface Rupture Zone
摘要
Abstract
On February 12, 2014, a Ms7.3 earthquake struck the eastern region of the West Kunlun Mountains in Yutian County, Xinjiang. Immediate (Feb 20th) field investigation following the earthquake shows that it produced surface ruptures at an altitude of 4600~5100 m. The surface rupture zone consists of a series of en-echelon tensional, shear-tensional to shear cracks, mole-tracks, and sag ponds. Striking NEE-SWW with a total length of about 25 km, the surface rupture zone is characterized by left-lateral strike slip motion with normal component. Maximum sinistral displacement along the surface rupture zone is about 1 m. What is particularly interesting here is that the surface rupture is distributed along two parallel faults, the Ashikule-Xor Kol fault and the south Xor Kol fault, which is rarely seen. The seismogenic fault of the earthquake is one splay at the southwestern end of the Altun fault. This fault combined with the Gozha Co fault and the Longmu Co fault constitutes a“new Altun fault”.关键词
于田/地震/2014/野外调查/地表破碎带Key words
Yutian/earthquake/2014/field study/surface rupture zone分类
天文与地球科学引用本文复制引用
李海兵,孙知明,潘家伟,刘栋梁,张佳佳,李成龙,刘亢,云锟,龚正..2014年于田Ms7.3地震野外调查--特殊的地表破裂带[J].地球学报,2014,(3):391-394,4.基金项目
本文由国家自然科学基金(编号:41202156)和中国地质调查局地质大调查项目(编号:1212011121267)联合资助。 （编号:41202156）
