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Correlation between movement of tectonicblocks and earthquakes in groups
作者姓名:范俊喜  马瑾  刁桂苓  单新建
作者单位:FAN Jun-xi1,2) () MA Jin1,2) () DIAO Gui-ling3) () SHAN Xin-jian1,2) () 1) Institute of Geology,China Seismological Bureau,Beijing 100029,China 2) Tectonophysics Laboratory,China Seismological Bureau,Beijing 100029,China 3) Seismological Bureau
基金项目:Foundation item: State Key Basic Research Planning Project (G199804070401).
摘    要:Introduction ZHANG and ZHONG (1977), ZHANG, et al (1978) and ZHANG (1984) pointed out that Chinese mainland is divided into two parts by the NS-trending tectonic belt, i.e., the eastern area and the western area, and each area is divided into tectonic blocks by faults. In the eastern area, the faults are trending NNE and NNW, mainly NNE, and the long axis strike of blocks is nearly trending NS. In the western area, faults are trending NEE and NWW, mainly NWW, long axis strike …

收稿时间:2 April 2001
修稿时间:9 September 2001

Correlation between movement of tectonic blocks and earthquakes in groups
FAN Jun-xi,MA Jin,DIAO Gui-ling,SHAN Xin-Jian.Correlation between movement of tectonicblocks and earthquakes in groups[J].Acta Seismologica Sinica(English Edition),2001,14(5):547-555.
Authors:FAN Jun-xi  MA Jin  DIAO Gui-ling  SHAN Xin-Jian
Institution:1. Institute of Geology, China Seismological Bureau,
2. Seismological Bureau of Hebei Province,
Abstract:The Chinese mainland is divided into some tectonic blocks by nearly NE- and EW-orientated faults. Meanwhile strong earthquakes in the Chinese mainland usually cluster in time and space. We call earthquakes in groups. Tectonic blocks separated by faults and earthquakes in groups are prominent features of the tectonics of the Chi-nese mainland. Correlation between movement of tectonic blocks and groups of earthquakes is discussed in this paper. The results show that earthquakes in groups often occurred at one or several block boundary faults. The released elastic strain energy is built up in the same periods and around blocks. It means that strong earthquakes in groups are mainly caused by movement of blocks. Four types of block movement are identified based ongroup earthquakes: movement along a single boundary of a block (or a combined blocks), movement of a single block, movement of multi-blocks, and movement in block interiors. If we consider distribution of all strong earthquakes occurred in the Chinese mainland, the movement along a single boundary of a block is more popular one inducing strong earthquakes. But if we only consider earthquakes in groups rather than single earthquakesthe movement of a block dominates among four modes. Statistics with respect to group earthquakes show that the Taihangshan mountain and the North China block are much active in the eastern part of Chinese mainland, and in western part of Chinese mainland the active blocks are Sichuan-Yunnan and the Kunlun-Songpan ones.
Keywords:tectonic block  earthquakes in groups  types of block movement
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