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《Chinese Journal of Sinica》 1977-02
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THE YONGSHAN(永善)-DAGUAN(大关) EARTHQUAKE (M=7.1) ON MAY 11, 1974.

LIU ZHENG-KONG LEI SU-HUA HU SU-HUA(Seismological Brigade of Kunming, National Seismological Bureau)  
In this paper, the seismo-tectonic structure associated with the occurrence of the Yongshan (永善)-Daquan (大关) Earthquake, M=7.1, on May 11, 1974 in Yunnan Province is discussed. It has been pointed out that the main shock was caused by at least two separate fractures on a fault striking N34°W and dipping to the northeast. The direction of fracturing was from southeast toward the northwest. However, the fault associated with the strongest aftershock of June 15 has a strike of N40°E and dip to the southeast. Just before the occurrence of this aftershock, the rate of strain release greatly increased and at the same time epicenters lined up along a definite direction.
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