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一般认为,喜马拉雅大地震很少造成地表破裂。然而,在尼泊尔的野外分析发现,至少1255年和1934年两次历史地震沿印度和亚洲边界的主断裂产生了大规模地表位移。
It is generally accepted that earthquakes rarely cause surface damage in the Himalayan Earthquake. However, a field analysis in Nepal found that at least the major faults along the Indian and Asian border between two historic earthquakes in 1255 and 1934 produced large-scale surface displacements.