滇西北断裂带痕量氢地震异常特征分析及预报效能评价OA
Seismic Anomaly Characteristics and Prediction Efficiency Evaluation of Trace Hydrogen in the Fault Zone of Northwestern Yunnan
在滇西北地区4个断裂带痕量氢观测点近5 a全时段高精度连续观测数据统计分析、相关性拟合及预处理的基础上,对观测数据开展地震预报效能评价,并结合效能评价结果与前人研究结果分析痕量氢浓度地震异常特征及原因.结果表明:1)滇西北地区温泉逸出氢气浓度变化与气温、气压具有一定的相关性,呈现出明显的年变特征,而土壤逸出氢气则与气象要素基本不相关;对比前人研究表明,断裂带痕量氢浓度规律具有显著的空间异质性,其受控因素并非单一模式.2)滇西北地区4个痕量氢观测点均为具有统计检验意义的有效地震预测指标,其中土壤逸出氢气短期预测效果更好,可信度却较低;温泉逸出氢气的预测效能则以中长期为主,可信度较高.3)滇西北地区断裂带氢气异常与地震活动密切相关,地震前兆异常通常表现为突然增高或锯齿状起伏;由于氢气来源、逸出过程和不同地区地储温度等存在差异,温泉逸出氢气与土壤逸出氢气的地球化学背景值同样具有显著的空间异质性.
Based on the statistical analysis,correlation fitting and preprocessing of high-precision con-tinuous observation data of four trace hydrogen observation points in fault zones of northwestern Yun-nan over the past five years,we evaluate the seismic prediction efficiency of observational data,and analyze the characteristics and causes of trace hydrogen concentration anomalies related to earthquakes combining with previous studies.The results show that:1)The concentration variations of hydrogen escaping from hot springs in northwestern Yunnan are correlated with temperature and air pressure,showing distinct annual variation features.In contrast,hydrogen escaping from soil is essentially un-correlated with meteorological elements.Comparison with previous studies,there is a significant spa-tial heterogeneity in the distribution of trace hydrogen concentration in fault zones,which is not con-trolled by a single factor.2)All of four trace hydrogen observation points in northwestern Yunnan are effective seismic prediction indicators with statistical significance.The short-term prediction effect of hydrogen escaping from soil is better but with relatively lower credibility.The prediction efficiency of hydrogen escaping from hot springs is mainly in medium to long term,with relatively higher credibili-ty.3)There is a close correlation between hydrogen anomalies in fault zones and seismic activities in northwestern Yunnan.Seismic precursory anomalies typically manifest as sudden increases or saw-tooth fluctuations.Due to differences in hydrogen sources,escaping processes,and geothermal stor-age temperatures in different regions,the geochemical background values of hydrogen escaping from hot springs and soil also exhibit significant spatial heterogeneity.
黑贺堂;张源;李庆;高琼;匡泳庄;李梅芳;邓嘉美
中国地震科学实验场大理中心,大理,671000||云南大理滇西北地壳构造活动野外科学观测研究站,大理,671000中国地震科学实验场大理中心,大理,671000中国地震科学实验场大理中心,大理,671000中国地震科学实验场大理中心,大理,671000云南省地震局,昆明,650224玉龙县地震局,丽江,674100中国地震科学实验场大理中心,大理,671000
天文与地球科学
断裂带痕量氢效能评价异常特征
fault zonetrace hydrogenefficiency evaluationabnormal characteristics
《大地测量与地球动力学》 2026 (1)
106-114,9
中国地震局震情跟踪定向工作任务(2024010312)中国地震局"三结合"课题(3JH-202401094).
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