In the Xindukushi region, the focus offsets are mainly the form of dip-slip thrusts, the elevation angles of axis T almost vertical;
兴都库什地区震源断错以倾滑道断层为主,T轴仰角几乎垂直。
In the Xindukushi region, the focus offsets are mainly the form of dip-slip thrusts, the elevation angles of axis T almost vertical;
兴都库什地区震源断错以倾滑道断层为主,T轴仰角几乎垂直。
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