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Asthenosphere and Plates of Northeast Asia

机译:东北亚软流圈和板块

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摘要

In the territory of Northeast Asia north of latitude 56, the three largest lithospheric plates (Eurasian, North American, and Pacific) and some plates of second rank (Amur, Sea of Okhotsk, and Sea of Bering) are conjugated and their space-time interrelations are the subject of heated discussions. Tectonists diagnose boundaries and kinematic characteristics of plates proceeding from analysis of the tectonostratigraphic, paleogeo-graphic, magmatic, and structural attributes observed in a thin superficial layer of the crust. Works of seismologists are based on the spatial distribution of centers of earthquakes and calculations of vectors of seismotectonic pressures in fields of strong seismic events. These systems of estimations do not always coincide during the characterization of spatial parameters and evolution of the lithospheric plates. In particular, the site of the modern boundary between the Eurasian (EAP) and North American (NAP) plates varies by more than 700 km in different estimations.
机译:在北纬56以北的东北亚领土中,三个最大的岩石圈板块(欧亚大陆,北美和太平洋)和一些第二等级的板块(阿穆尔,鄂霍次克海和白令海)被共轭并且其时空共轭相互关系是激烈讨论的主题。构造学家通过对地壳薄表层中观察到的构造地层学,古地貌学,岩浆学和结构属性进行分析,从而诊断板块的边界和运动学特征。地震学家的工作是基于地震中心的空间分布以及在强地震事件领域中地震构造压力矢量的计算。在空间参数的表征和岩石圈板块的演化过程中,这些估算系统并不总是一致的。特别是,欧亚大陆(EAP)和北美(NAP)板块之间现代边界的位置在不同估计中相差700多公里。

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