ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
大陆漂移, 板块构造, 地质力学
  
关键词:continental drift  plate tectonics  geomechanics  Li Siguang
基金项目:中国地质调查局项目“青藏高原深部结构探测与地壳活动特征”(编号:1212010511809)
作者单位E-mail
赵文津 中国地质科学院 zhaowj@cae.cn 
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摘要:
Continental Drift, Plate Tectonics and Geomechanics
      This paper briefly describes the major content and basis of Wegener’s continental drift hypothesis and deals with the fact that, due to the discovery of the mid-ocean ridge and the ocean floor expansion during the geological and geophysical survey on the basis of the continental drift hypothesis, researchers have explained the mechanism of continental tensional faulting and established the global plate tectonic theory, thus resulting in the revolution of modern geoscience thinking. Simultaneously with the emergence of the continental drift hypothesis, Li Siguang actively approached and dealt with the problem of continental crust horizontal movement and, in combination with the reality of China’s mainland, developed the theory of intracontinental collision deformation, i.e., the geomechanic theory and method that included the global continental tectonic system. Li Siguang emphasized that geomechanics studies the phenomena of crustal movement and deformation on the basis of geology on one side and mechanics on the other side. Later, he extended the application of geomechanics to the aspects of resources and environment. This paper makes a thorough discussion on the relationships between Wegener’s continental drift hypothesis, global plate tectonic theory and geomechanics, expounds the practical significance and fore-sight significance of Li Siguang’s geomechanic theory and method and puts forward the suggestion that we should attach great importance to and carry forward the valuable heritages that Li siguang left to us, deeply study Li Siguang’s works and, in combination with new achievements of geological survey, enrich and develop his theory.
ZHAO Win-jin.2009.Continental Drift, Plate Tectonics and Geomechanics[J].Acta Geoscientica Sinica,30(6):717-731.
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