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Background of crustal movement of Chinese mainland
      
Based on GPS data during May 1995-March 1998 of 12 IGS stations located in the Chinese mainland and its surrounding areas, the horizontal displacement rates of these IGS stations have been determined.
      
The result can be available to study the background of the crustal tectonic motion in the Chinese mainland.
      
PWV change in the Chinese mainland in 2004 is graphed with the gridding method of splines in tension, according to the GPS data of the crust monitor observation network in China, combined with relevant meteorology information.
      
In order to address this issue, we must endeavor to understand more clearly the prehistoric cultures of the southeastern coast of the Chinese mainland, and especially changes in settlement and subsistence patterns.
      
The Government of China is planning a new economic-development area, located at Meizhou Bay on the Chinese mainland, opposite the island of Taiwan.
      
Movement and strain conditions of active blocks in the Chinese mainland
      
The active blocks in the Chinese mainland have a consistent E-trending movement component, but its N and S components are not consistent.
      
It can be seen from superficial strain that the Chinese mainland is predominated by superficial expansion.
      
Almost the total area in the eastern part of the Chinese mainland is expanded, while in the western part, the superficial compression and expansion are alternatively distributed from the south to the north.
      
The mutual action of India, Pacific and Philippine Sea plates versus Eurasia plate is the principal driving force to the block movement in the Chinese mainland.
      
Inversion of waveform from the data of six moderate strong earthquakes in Chinese mainland to seismic moment tensors and source
      
Six moderately strong earthquakes which occurred in Chinese mainland in the past few years are studied.
      
Grouping occurrences being the fundamental feature of the strong earthquakes in Chinese mainland
      
The grouping occurrences of the strong earthquakes of Chinese mainland has been determined as a fundamental feature of the seismicity.
      
Research on the completeness of earthquake data in the Chinese mainland (I) - North China
      
Research on completeness of earthquake data in the Chinese mainland (II) - The regional distribution of the beginning years of b
      
Finally, we gave the regional distribution of the beginning years since which the data for different magntiude intervals are largely complete in the Chinese mainland.
      
The characteristics of tectonic stress field about strike slip earthquake-generating structure in the Chinese mainland
      
This paper is one of the series papers about the study on strike-slip earthquake-generating structure in the Chinese mainland.
      
 

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