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《Chinese Journal of Sinica》 1977-02
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PRESENT TECTONIC STRESS FIELD AND ITS RELATION TO THE CHARACTERISTICS OF RECENT TECTONIC ACTIVITY IN SOUTHWESTERN CHINA

KAN RONG-JU ZHANG SI-CHANG YAN FENG-TONG YU LIN-SHENG(The Seismological Brigade of Kunming, National Seismological Bureau)  
Based on the analysis of the focal mechanism solutions of 51 earthquakes occur-ing in Southwestern China and geological data of 10 earthquake fault zones of the region, we discuss in this paper, division of the present tectonic stress field in Souh-western China into separate regions and their relation to the recent tectonic activity.It has been found that a tectonic block in the shape of an inclosed rhomb bounded by the Xianshuihe (鲜水河), Anninghe (安宁河), Xiaojiang (小江), Qujiang (曲江) and Red River on the east, south and southwest, is moving southeastward relative to the surroundings. This rhmobic block controls the occurrence of most of the earthquakes in this area.
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