ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
全球级三个地震构造系统和大地水准面
  
关键词:seismotectonic system geoid antisymmentry global tectonics,
基金项目:
作者单位
马宗晋 国家地震局地质研究所 
高祥林 国家地震局地质研究所 
摘要点击次数: 2117
全文下载次数: 1962
摘要:
Three Seismotectonic Systems of the Global Scale and the Geoid
      Based on the comprehensive studies of the global sesmicity and active tectonics, the global seismotectonics is summarized with three great systems:(1)the circum-Pacific seismotectonicsystem of deep subduction(the P system);(2)the Atlantic seismotectonic system of mid-oceanic ridge rifts(the A system );and(3)the continental seismotectonic system of shear nets(the C system).There is important dynamic correlation between the distribution of these three systems on the earth’s surface and the deflection of the geoid relative to the ideal roatating ellipsoid.Comparative analyses are made for the three systems by using the data of tectonic deformation and earthquake mechanism. The A system is characterized by planar extensional fractures. The P system demonstraces obduction and overthrusting of the Atlantic(0°)hemisphere lithosphere to the Pacific(180°)hemisphere lithosphere. The A system representsdilatation of the south hemisphere ,while the C system indicates contraction of the northhemisphere. The relationship between the circum-antarctic oceanic ridge and the C system isprobably assoriated with the longitudinal flow of the mantle.
MA Zong-jin,GAO Xiang-lin.1994.Three Seismotectonic Systems of the Global Scale and the Geoid[J].Acta Geoscientica Sinica,15(3,4):97-102.
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