因此,鲜水河断裂带的石棉县地带已经被锁定为在未来可能会产生强震。
Hence, the Shimian section of the Xianshuihe fault zone is speculated to be currently locked and have the possibility of producing strong earthquake in the future.
因此,基于断裂带整体强震复发间隔分布的中长期危险性概率评估仍然面临一定的困难。
Therefore, the probabilistic assessment of middle - and long-term seismic hazard based on the strong earthquake recurrence for entireties of active fault zones still faces some difficulty.
这项研究成果将为评价龙门山断裂带余震和今后强震发展趋势提供关键构造物理参数。
These results provide key appraisal for future assessments of earthquake hazards of the Longmenshan fault zone and aftershock occurrences.
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