cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ck; mso-font-kerning: 18.0pt" lang=EN-US>ce="Times New Roman">The Relation Between H2 Release and Earthquake and Block Structure in ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">HeilongjiangceName> ceType w:st="on">ProvinceceType>ce>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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摘要

cm 0cm 0pt" class=MsoNormal>///In this paper, the authors studied the block-structured basement, the Mesozoic-Cenozoic faults, and the deep upwelling asthenosphere as the structural background of earthquakes in ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">HeilongjiangceName> ceType w:st="on">ProvinceceType>ce>, using geophysical data of different depths. The features of the seismic activities in the concerned area different from those in the western country-region w:st="on">ce w:st="on">Chinace>country-region> are also related to the features of the fault activities here that can be interpreted by the fact that the eastern Chinese-Mongolian region is creeping eastwards as shown by the GPS vector field.ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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