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切尔斯基地震带是东北亚的宽400公里的北西向震中带(图1),东南伸向科尔多曼群岛,西北到达拉普捷夫海。我们不同意通常被认可的有关该地震带地球动力学的观点,许多工作者将Gakkel山脉至日本岛弧北
The Cherskii seismic belt is a 400-kilometer-wide NW-trending epicenter belt in northeast Asia (Fig. 1), southeastern to the Kordurman Islands, and to the northwest to the Laptev Sea. We disagree with the commonly accepted view of the geodynamics of the seismic zone that many workers have moved the Gakkel Range to the northern tip of Japan Island Arc North