结果表明，四川地区强震的发震机制与区域断裂类型及其活动方式有着十分密切的联系。
The results show that the occurring mechanism of strong earthquakes has a very close correlation with the type and active manner of regional fault in Sichuan region.
类型上，断裂主要有正断层、逆断层和雁行断层等形式。
On type, the fractures appear normal fault, strike-slip fault and so on.
准噶尔盆地南缘的构造样式类型以断裂和褶皱的各种组合类型为主。
The tectonic patters of south margin of Junggar basin are composed of the composition of faults and folds mostly.
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