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在1970年苏联的正式地震区划图上,亚美尼亚中部和西南部地区,整个都划为8度区。这些图件是根据地震资料编制的,主要方法是把已知地震在平面上的分布联系起来。地震区划的另一种方法是1949年就已提出的新型的地震构造图,图上表示了地震发生带。地震发生带是根据综合资料,其中包括地质资料确定的,表示任何一个强度最大的地震可能发生的地带。一、地质构造在亚美尼亚境内的地质构造中,有前寒武系-下古生界、古生界、中生
In the 1970 Soviet official earthquake zoning map, the central and southwestern Armenia, the entire area is classified as 8 degrees. The maps are based on seismic data and the main method is to relate the distribution of known earthquakes in the plane. Another method of seismic zoning is the new seismic structure that was proposed in 1949 and shows the seismic zone. Seismogenic zones are based on a combination of data, including those determined by geological data, that indicate the likely occurrence of any one of the strongest earthquakes. First, the geological structure In the geological structure in Armenia, the Precambrian - Lower Paleozoic, Paleozoic, Mesozoic