地震发生的北安纳托尼亚平移断层带，大约沿伊兹·米特湾呈东西向分布。
The earthquake occurred along the North Anatolian strike-slip fault that extends roughly east-west beneath the Gulf of Izmit.
其他断层带地区的进展情况参差不齐：设想令人鼓舞，但进展却不尽如人意。
The same stark contrast prevails in other fault zones: encouraging ideas, discouraging progress.
此外，25英里长的断层带正好通过唐山，唐山的建筑物结构很少具有抗震性。
Furthermore, a 25-mile long fault passes through Tangshan, where only few of its structures are earthquake-resistant.
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