大陆板内塑性流动波与地震迁移(二)
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摘要
基于大陆岩石圈塑性流动网络和塑性流动波的观念,地震迁移主要表现为塑性流动波控制下地震沿网带的迁移。中东亚网络系统存在着两种以上的塑性流动波,其中与地震中期预测有关的是“十年波”和“百年波”。它们具有不同的起波年份、起波期和波峰带,而各期波的优势传播方向和有效作用范围又有所不同。两种波的波峰带相互叠合形成双重波峰区,其中有“塑性流动-地震”网带经过的区段为地震提供必要的能量背景条件,构成能量背景区。对中国大陆1976年震情的检验表明,6.0~7.8级地震共19次,约有90%分布在相应震级范围的能量背景区内。
Based on the concepts of plastic-flow network and plastic-flow waves in the continentallithosphere, migration of earthquakes is essentially their moving along”plastic-flow/seismic”belts in network system controlled by the plastic-flow waves. In terms of the inference from thetime-space distribution of earthquakes, there are at least two sorts of plastic-flow waves in thecentral and eastern Asian network svstem, such as the“decade-wave” and” century-wave” in-volving the interrnediate- range prediction of earthquakes. They are of different wave-originatedtimes, wave-originated stages, and wave-crest belts,and different preferential propagation direc-tions and effective action ranges for each stage. The overlapping of the two sorts of wave-crestbelts forms the double wave-crest areas in which the portion covered by ” plastic-flow/seismic”belts becomes the energy background areas necessary for earthquakes. It is indicated by examin-ing the situation in 1976 that about 90%of 19 earthquakes with magnitudes ranging 6.0 to 7.9,or about 83%of 6 groups of these earthquakes,distribute in the energy background areas withthe corresponding earthquake magnitude ranges.
引文
1王绳祖.大陆岩石圈的网络状塑性流动、塑性波和地震活动。见:国家地震局地质研究所编:现今地球动力学研究及其应用。北京:地震出版社,1994.20~27。2王绳祖。亚洲大陆岩石圈多层构造模型和塑性流动网络。地质学报,1993,67(1):1~18。3王绳祖,张宗淳。大陆板内塑性流动波与地震迁移(一)地震地质,1994,16(4):289~297。4邓志辉,马瑾。地震活动和大地构造的特征尺度。地球物理学进展,1993,8(4):104~110。5杜品仁,徐道一。天文地震学。北京:地震出版社,1989。6王绳祖。浅源强震的判据和发震概率.地震地质,1990,12(2):131~140。7王绳祖。青藏高原中部地区潜在震源发震概率的构造物理方法研究。地震地质,1993,15(1):1~20。

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