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强烈地震源(M≥6)位于厚度大于10 km的活动地幔层下伏的造山带范围内,天山和高加索地下输送的热柱通道位置不一,这种因素和固结地壳构造的区域差别都影响地震活动的最大能量水平。
Strong source (M≥6) is located in the range of orogenic belts below the active mantle below 10 km in thickness. The locations of the hot column channels transported underground by Tianshan and Caucasus are different from those of the consolidated crust The maximum energy level that affects seismic activity.