GLOBAL SEISMOTECTONIC SYSTEMS AND THE EARTH'S ASYMMETRY--《中国科学B辑(英文版)》1990年01期

《中国科学B辑(英文版)》 1990-01

GLOBAL SEISMOTECTONIC SYSTEMS AND THE EARTH'S ASYMMETRY

MA ZONG-JIN AND CHEN QIANG (Institute of Geology, State Seismological Bureau, Beijing 100011, PRC)

This paper mainly discusses the relation between global seismotectonic systems and asymmetric geodynamic systems. Global seismotectonic systems may be divided into three asymmetric I-Scale systems: the circum-Pacific seismotectonic system, the oceanic ridge seismotectonic system, and the continental seismotectonic system in the Northern Hemiaphere. Global asymmetry is also indicated by the asymmetry between the Southern and Northern Hemispheres, the asymmetry between the Atlantic and Pacific Hemispheres, and the asymmetry between the east and west of meridioual tectonics. Global asymmetric geodynamic systems may be composed of meridional convection, latitudinal convection, and inertia flow resulting from the variation of the Earth's rotational velocity. These geodynamic systems constitute the dynamic background of global asymmetry and control the frameworks of global seismotectonic systems.

【Key Words】： seismotectonic system geodynamic system asymmetry torsion of hemispheres inertia flow.

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