我国地形变场的统计特征及与地温场的相关
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摘要
利用1986~1990年我国大陆42°N以南,97°E以东共41个站的地倾斜资料,内插到经纬度1°×1°的网格上,可求得各月的地形变场,由此分析得到地凸区、地凹区、鞍形区、半鞍形区等形变特征场。结果表明:在逐月的地形变场上,一般有4~5个地凸区和地凹区,其平均水平尺度约400km,单体生命史大约3.5季;地凸/凹区中心与地震活动带基本一致。另外,地凸区与地热涡,地凹区与地冷涡有很好的对应,此结果支持了文献〔8〕提出的地气耦合的概念模式。
Interpolating the ground tilt data in mainland (south to 45°N, east to 97°E, totally 41stations)during 1986 to 1990 into grid points of 1°×1°, the monthly earth surface deformation field was calculated. Some characteristics of deformation field can be identified from it including convex area、concave area and saddle area, etc. The results show that there are usually 4~5 convex and concave areas respectively on monthly or seasonal deformation field with an average horizontal scale of 400 km or so and a life span of 3.5 seasons approximately. The concentration region of centers of convex/concave areas consists with the earthquake belts. Moreover, the convex area is well corresponding to the “Underground hot vortex”while the concave area is in good agreement with “Underground cold vortex”, which strongly supports the conceptual model indicating the couple between the earth and the atmosphere proposed in Reference 8 .
引文
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