Article(id=1322566812546482996, tenantId=1146029695717560320, journalId=1281212831689347082, issueId=1322566763112415546, articleNumber=null, orderNo=null, doi=10.14075/j.jgg.2025.01.603, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1736352000000, receivedDateStr=2025-01-09, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1793254100213, onlineDateStr=2026-10-29, pubDate=1768406400000, pubDateStr=2026-01-15, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793254100213, onlineIssueDateStr=2026-10-29, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793254100213, creator=13701087609, updateTime=1793254100213, updator=13701087609, issue=Issue{id=1322566763112415546, tenantId=1146029695717560320, journalId=1281212831689347082, year='2026', volume='46', issue='1', pageStart='1', pageEnd='138', issueExtLink='null', onlineDate='null', pubDate='1768406400000', pubDateStr='2026-01-15', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1793254088427, creator='13701087609', updateTime=1793254088427, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=106, endPage=114, ext={EN=ArticleExt(id=1322566812739420981, articleId=1322566812546482996, tenantId=1146029695717560320, journalId=1281212831689347082, language=EN, title=Seismic Anomaly Characteristics and Prediction Efficiency Evaluation of Trace Hydrogen in the Fault Zone of Northwestern Yunnan, columnId=null, journalTitle=Journal of Geodesy and Geodynamics, columnName=null, runingTitle=null, highlight=null, articleAbstract=
Based on the statistical analysis, correlation fitting and preprocessing of high-precision continuous observation data of four trace hydrogen observation points in fault zones of northwestern Yunnan 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 uncorrelated with meteorological elements. Comparison with previous studies, there is a significant spatial heterogeneity in the distribution of trace hydrogen concentration in fault zones, which is not controlled 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 credibility. 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 sawtooth fluctuations. Due to differences in hydrogen sources, escaping processes, and geothermal storage temperatures in different regions, the geochemical background values of hydrogen escaping from hot springs and soil also exhibit significant spatial heterogeneity.
, authors=Hetang HEI
1, 2, Yuan ZHANG
1, Qing LI
1, Qiong GAO
1, Yongzhuang KUANG
3, Meifang LI
4, Jiamei DENG
1, authorsList=Hetang HEI, Yuan ZHANG, Qing LI, Qiong GAO, Yongzhuang KUANG, Meifang LI, Jiamei DENG, authorCompany=null, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=
All rights reserved. Unauthorized reproduction is prohibited., copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1322566814253564738, articleId=1322566812546482996, tenantId=1146029695717560320, journalId=1281212831689347082, language=CN, title=滇西北断裂带痕量氢地震异常特征分析及预报效能评价, columnId=1281933709121138897, journalTitle=大地测量与地球动力学, columnName=地球动力学, runingTitle=null, highlight=null, articleAbstract=
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。
, authors=黑贺堂
1, 2, 张源
1, 李庆
1, 高琼
1, 匡泳庄
3, 李梅芳
4, 邓嘉美
1, authorsList=黑贺堂, 张源, 李庆, 高琼, 匡泳庄, 李梅芳, 邓嘉美, authorCompany=null, correspAuthors=null, authorNote=
, correspAuthorsNote=null, copyrightStatement=
版权所有，未经授权，不得转载。, copyrightOwner=大地测量与地球动力学编辑部, extLink=null, articleAbsUrl=null, sourceXml=FYQeOgvyXcVupD9ELeuDLw==, magXml=WXABYZL8D32sGTwJf/VFQg==, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=aPrYe1/JBY11eDCYJbokkA==, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=RW7lSg80isD9xa65Io9IXQ==, mapNumber=null, fund=null)}, authors=[Author(id=1322566814966596432, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=854360354@qq.com, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322566815050482515, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, authorId=1322566814966596432, language=EN, stringName=Hetang HEI, firstName=Hetang, middleName=null, lastName=HEI, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
1, 2, address=1 Dali Center of China Earthquake Science Experimental Field, Dali 671000, China
2 Field Scientific Observation and Research Station on Crustal Tectonic Activities in Northwestern Yunnan, Dali 671000, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1322566815142757204, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, authorId=1322566814966596432, language=CN, stringName=黑贺堂, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
1, 2, address=1 中国地震科学实验场大理中心, 大理, 671000
2 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, bio={"content":"
黑贺堂, 工程师, 主要从事地震监测预报与地震地质研究, E-mail: 854360354@qq.com
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黑贺堂, 工程师, 主要从事地震监测预报与地震地质研究, E-mail: 854360354@qq.com
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Main geological structures, location of hydrogen observation points, and distribution of ML ≥ 3.0 earthquakes in the study area from January 2019 to December 2023, figureFileSmall=bGYz/Nq9zlHEQn07otoNsA==, figureFileBig=aPrYe1/JBY11eDCYJbokkA==, tableContent=null), ArticleFig(id=1322566817474790268, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=图1, caption=
研究区主要地质构造、氢气观测点位置及2019-01-2023-12 ML≥3.0地震分布, figureFileSmall=bGYz/Nq9zlHEQn07otoNsA==, figureFileBig=aPrYe1/JBY11eDCYJbokkA==, tableContent=null), ArticleFig(id=1322566817718059901, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Fig. 2, caption=
Structure of the observation devices, figureFileSmall=Pe9ihQ2cEFbjsBx4RdNhKw==, figureFileBig=AkQVk7yq9fB9sQObAOC68A==, tableContent=null), ArticleFig(id=1322566817814528894, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=图2, caption=
观测装置结构, figureFileSmall=Pe9ihQ2cEFbjsBx4RdNhKw==, figureFileBig=AkQVk7yq9fB9sQObAOC68A==, tableContent=null), ArticleFig(id=1322566817890026367, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Fig. 3, caption=
Distribution of hydrogen concentration measurement values, figureFileSmall=l6+zzMx1XcMPmt6iFGeAAA==, figureFileBig=5VSP/q5ZML1/WiDqUp9l4Q==, tableContent=null), ArticleFig(id=1322566817986495360, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=图3, caption=
氢浓度测值分布, figureFileSmall=l6+zzMx1XcMPmt6iFGeAAA==, figureFileBig=5VSP/q5ZML1/WiDqUp9l4Q==, tableContent=null), ArticleFig(id=1322566818053604225, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Fig. 4, caption=
Original hydrogen concentration variation curves of four monitoring points and preprocessed variation curves of hot spring gases, figureFileSmall=EnFZyfe6OpKnX/NIw6PmHA==, figureFileBig=rEMdHKBn2bYzoVAauglwHA==, tableContent=null), ArticleFig(id=1322566818120713090, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=图4, caption=
4个观测点氢气浓度原始变化曲线及温泉气预处理变化曲线, figureFileSmall=EnFZyfe6OpKnX/NIw6PmHA==, figureFileBig=rEMdHKBn2bYzoVAauglwHA==, tableContent=null), ArticleFig(id=1322566818187821955, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Fig. 5, caption=
The multi-year periodic component of trace hydrogen concentration in northwestern Yunnan, figureFileSmall=7nvyeuZxiqdrel2BOasQPQ==, figureFileBig=K25u/3cp/VDfTQ/5P3/9IQ==, tableContent=null), ArticleFig(id=1322566818263319428, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=图5, caption=
滇西北地区痕量氢浓度多年周期成分分析结果, figureFileSmall=7nvyeuZxiqdrel2BOasQPQ==, figureFileBig=K25u/3cp/VDfTQ/5P3/9IQ==, tableContent=null), ArticleFig(id=1322566818355594117, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Fig. 6, caption=
Results of Molchan test, figureFileSmall=7XKL7OrE9lobkDb+l4bi9A==, figureFileBig=bCt98m+b3UJeIP3mmVeMIg==, tableContent=null), ArticleFig(id=1322566818452063110, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=图6, caption=
Molchan检验结果, figureFileSmall=7XKL7OrE9lobkDb+l4bi9A==, figureFileBig=bCt98m+b3UJeIP3mmVeMIg==, tableContent=null), ArticleFig(id=1322566818523366279, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Tab. 1, caption=
Catalog of earthquakes with MS≥4.0 in northwestern Yunnan
, figureFileSmall=null, figureFileBig=null, tableContent=
| 序号 | 发震时间 | 震中位置 | 发震地点与震级 | 重定位深度/km | 发震类型 |
| 经度/(°) | 纬度/(°) |
| 1 | 2019-02-02 | 100.93 | 27.12 | 宁蒗县4.5 | 15 | 走滑型 |
| 2 | 2019-07-21 | 100.62 | 26.17 | 永胜县4.8 | 10 | 走滑型 |
| 3 | 2019-11-25 | 99.70 | 25.97 | 洱源县4.7 | 12 | 走滑型 |
| 4 | 2021-05-13 | 99.23 | 24.43 | 漾濞县4.6 | 8 | 走滑型 |
| 5 | 2021-05-21 | 99.87 | 25.67 | 漾濞县6.4 | 8 | 走滑型 |
| 6 | 2022-01-02 | 100.65 | 27.78 | 宁蒗县5.5 | 10 | 走滑型 |
| 7 | 2022-09-23 | 98.77 | 24.78 | 龙陵县4.7 | 9 | 走滑型 |
| 8 | 2023-05-02 | 99.28 | 25.35 | 隆阳区5.2 | 10 | 走滑型 |
| 9 | 2023-12-02 | 98.08 | 24.27 | 芒市5.0 | 10 | 走滑型 |
), ArticleFig(id=1322566818594669448, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=表1, caption=
滇西北地区MS≥4.0地震目录
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| 序号 | 发震时间 | 震中位置 | 发震地点与震级 | 重定位深度/km | 发震类型 |
| 经度/(°) | 纬度/(°) |
| 1 | 2019-02-02 | 100.93 | 27.12 | 宁蒗县4.5 | 15 | 走滑型 |
| 2 | 2019-07-21 | 100.62 | 26.17 | 永胜县4.8 | 10 | 走滑型 |
| 3 | 2019-11-25 | 99.70 | 25.97 | 洱源县4.7 | 12 | 走滑型 |
| 4 | 2021-05-13 | 99.23 | 24.43 | 漾濞县4.6 | 8 | 走滑型 |
| 5 | 2021-05-21 | 99.87 | 25.67 | 漾濞县6.4 | 8 | 走滑型 |
| 6 | 2022-01-02 | 100.65 | 27.78 | 宁蒗县5.5 | 10 | 走滑型 |
| 7 | 2022-09-23 | 98.77 | 24.78 | 龙陵县4.7 | 9 | 走滑型 |
| 8 | 2023-05-02 | 99.28 | 25.35 | 隆阳区5.2 | 10 | 走滑型 |
| 9 | 2023-12-02 | 98.08 | 24.27 | 芒市5.0 | 10 | 走滑型 |
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Evaluation results of prediction efficiency
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| 观测点 | 预测窗长/d | 阈值倍率 | R | R0 | 效能检验 | 报对次数 | 虚报次数 | 漏报次数 | 漏报率/% |
| 汝南 | 30 | 1.3 | 0.141 0 | 0.247 7 | 未通过 | 2 | 3 | 5 | 71.4 |
| 60 | 1.0 | 0.460 1 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 80 | 1.2 | 0.461 3 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 120 | 1.2 | 0.413 6 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 150 | 1.4 | 0.413 6 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 180 | 1.2 | 0.390 6 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 360 | 2.4 | 0.342 9 | 0.386 4 | 未通过 | 4 | 0 | 3 | 42.9 |
| 洱源 | 30 | 1.2 | 0.500 7 | 0.555 0 | 未通过 | 3 | 1 | 1 | 25.0 |
| 60 | 1.4 | 0.558 0 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 90 | 1.5 | 0.581 9 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 120 | 1.6 | 0.581 9 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 150 | 1.7 | 0.581 9 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 170 | 1.1 | 0.605 3 | 0.601 0 | 通过 | 4 | 0 | 0 | 0 |
| 360 | 1.6 | 0.468 0 | 0.601 0 | 未通过 | 4 | 0 | 0 | 0 |
| 弥渡 | 30 | 1.2 | 0.446 5 | 0.452 0 | 未通过 | 3 | 2 | 2 | 40.0 |
| 50 | 1.2 | 0.453 7 | 0.452 0 | 通过 | 3 | 1 | 2 | 40.0 |
| 90 | 1.2 | 0.375 3 | 0.452 0 | 未通过 | 3 | 1 | 2 | 40.0 |
| 120 | 1.2 | 0.358 9 | 0.452 0 | 未通过 | 3 | 1 | 2 | 40.0 |
| 150 | 1.2 | 0.429 6 | 0.452 0 | 未通过 | 3 | 0 | 2 | 40.0 |
| 180 | 1.2 | 0.429 6 | 0.452 0 | 未通过 | 3 | 0 | 2 | 40.0 |
| 360 | 1.9 | 0.505 7 | 0.515 0 | 未通过 | 4 | 0 | 1 | 25.0 |
| 保山 | 30 | 2.8 | 0.113 2 | 0.137 8 | 未通过 | 1 | 1 | 6 | 85.7 |
| 60 | 2.4 | 0.242 2 | 0.247 7 | 未通过 | 2 | 0 | 5 | 71.4 |
| 90 | 1.2 | 0.342 1 | 0.423 2 | 未通过 | 5 | 3 | 2 | 28.6 |
| 120 | 1.2 | 0.276 7 | 0.423 2 | 未通过 | 5 | 3 | 2 | 28.6 |
| 150 | 1.8 | 0.246 0 | 0.328 5 | 未通过 | 3 | 1 | 4 | 57.1 |
| 180 | 1.5 | 0.531 1 | 0.435 1 | 通过 | 6 | 0 | 1 | 14.2 |
| 360 | 1.7 | 0.447 5 | 0.435 1 | 通过 | 6 | 0 | 1 | 14.2 |
), ArticleFig(id=1322566818749858698, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=CN, label=表2, caption=
预报效能评价结果
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| 观测点 | 预测窗长/d | 阈值倍率 | R | R0 | 效能检验 | 报对次数 | 虚报次数 | 漏报次数 | 漏报率/% |
| 汝南 | 30 | 1.3 | 0.141 0 | 0.247 7 | 未通过 | 2 | 3 | 5 | 71.4 |
| 60 | 1.0 | 0.460 1 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 80 | 1.2 | 0.461 3 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 120 | 1.2 | 0.413 6 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 150 | 1.4 | 0.413 6 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 180 | 1.2 | 0.390 6 | 0.386 4 | 通过 | 4 | 0 | 3 | 42.9 |
| 360 | 2.4 | 0.342 9 | 0.386 4 | 未通过 | 4 | 0 | 3 | 42.9 |
| 洱源 | 30 | 1.2 | 0.500 7 | 0.555 0 | 未通过 | 3 | 1 | 1 | 25.0 |
| 60 | 1.4 | 0.558 0 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 90 | 1.5 | 0.581 9 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 120 | 1.6 | 0.581 9 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 150 | 1.7 | 0.581 9 | 0.555 0 | 通过 | 3 | 0 | 1 | 25.0 |
| 170 | 1.1 | 0.605 3 | 0.601 0 | 通过 | 4 | 0 | 0 | 0 |
| 360 | 1.6 | 0.468 0 | 0.601 0 | 未通过 | 4 | 0 | 0 | 0 |
| 弥渡 | 30 | 1.2 | 0.446 5 | 0.452 0 | 未通过 | 3 | 2 | 2 | 40.0 |
| 50 | 1.2 | 0.453 7 | 0.452 0 | 通过 | 3 | 1 | 2 | 40.0 |
| 90 | 1.2 | 0.375 3 | 0.452 0 | 未通过 | 3 | 1 | 2 | 40.0 |
| 120 | 1.2 | 0.358 9 | 0.452 0 | 未通过 | 3 | 1 | 2 | 40.0 |
| 150 | 1.2 | 0.429 6 | 0.452 0 | 未通过 | 3 | 0 | 2 | 40.0 |
| 180 | 1.2 | 0.429 6 | 0.452 0 | 未通过 | 3 | 0 | 2 | 40.0 |
| 360 | 1.9 | 0.505 7 | 0.515 0 | 未通过 | 4 | 0 | 1 | 25.0 |
| 保山 | 30 | 2.8 | 0.113 2 | 0.137 8 | 未通过 | 1 | 1 | 6 | 85.7 |
| 60 | 2.4 | 0.242 2 | 0.247 7 | 未通过 | 2 | 0 | 5 | 71.4 |
| 90 | 1.2 | 0.342 1 | 0.423 2 | 未通过 | 5 | 3 | 2 | 28.6 |
| 120 | 1.2 | 0.276 7 | 0.423 2 | 未通过 | 5 | 3 | 2 | 28.6 |
| 150 | 1.8 | 0.246 0 | 0.328 5 | 未通过 | 3 | 1 | 4 | 57.1 |
| 180 | 1.5 | 0.531 1 | 0.435 1 | 通过 | 6 | 0 | 1 | 14.2 |
| 360 | 1.7 | 0.447 5 | 0.435 1 | 通过 | 6 | 0 | 1 | 14.2 |
), ArticleFig(id=1322566818833744779, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566812546482996, language=EN, label=Tab. 3, caption=
Trace hydrogen anomaly changes along fault zones in northwestern Yunnan and corresponding earthquakes
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| 观测点 | 研究地震 | 异常持续时间 | 震中距/km | 异常特征 |
| 汝南 | 2019-02-02宁蒗MS4.5 | 2019-01-05-2019-02-09 | 85 | 突升超出阈值高值-突降恢复-突升超出阈值高值-波动上升下降 |
| 2019-07-21永胜MS4.8 | 2019-06-24-2019-07-20 | 82 | 突升超出阈值高值-突降恢复-突升超出阈值高值 |
| 2019-11-25洱源MS4.7 | 2019-10-11-2019-10-26 | 102 | 突升超出阈值高值-突降恢复 |
| 2021-05-21漾濞MS6.4 | 无异常 | 115 | 无异常 |
| 2022-01-02宁蒗MS5.5 | 无异常 | 135 | 无异常 |
| 2023-05-02隆阳MS5.2 | 无异常 | 168 | 无异常 |
| 2023-12-02芒市MS5.0 | 2023-08-04-2023-10-20 | 300 | 突升超出阈值高值-突降恢复-突升超出阈值高值-突降恢复、波动幅度大 |
| 洱源 | 2021-05-21漾濞MS6.4 | 2021-02-21-2021-05-08 | 51 | 突降超出阈值低值-持续低值波动-突升恢复-突降超出阈值低值 |
| 2022-01-02宁蒗MS5.5 | 2021-10-18-2022-02-10 | 198 | 突升超出阈值高值-突降恢复-突升超出阈值高值-在高值波动上升下降 |
| 2023-05-02隆阳MS5.2 | 2023-02-08-2023-04-25 | 108 | 趋势下降超出阈值低值-持续低值波动-突升恢复 |
| 2023-12-02芒市MS5.0 | 2023-06-13-2023-06-18 | 279 | 突升超出阈值高值-突降恢复 |
| 弥渡 | 2019-07-21永胜MS4.8 | 2019-04-29-2019-07-23 | 94 | 突升超出阈值高值-持续高值波动-突降恢复-突升超出阈值高值 |
| 2019-11-25洱源MS4.7 | 2019-08-29-2019-11-24 | 99 | 突升超出阈值高值-突降恢复-突升超出阈值高值持续波动 |
| 2021-05-21漾濞MS6.4 | 2021-03-03-2021-03-31 | 68 | 突升超出阈值高值-突降恢复-突升超出阈值高值-突降恢复 |
| 2022-01-02宁蒗MS5.5 | 无异常 | 273 | 无异常 |
| 2023-12-02芒市MS5.0 | 无异常 | 265 | 无异常 |
| 保山 | 2019-11-25洱源MS4.7 | 2019-11-09-2019-11-27 | 106 | 突降超出最低阈值-突升恢复-突降超出最低阈值-突升恢复 |
| 2021-05-13漾濞MS4.6 | 2020-11-20-2021-05-09 | 78 | 突降超出最低阈值-突升恢复、震前数天又多次突升超出阈值高值波动上升下降 |
| 2021-05-21漾濞MS6.4 | 91 |
| 2022-01-02宁蒗MS5.5 | 2021-08-14-2021-12-23 | 300 | 多次突升超出阈值高值-震前数天突升超出阈值-突降恢复 |
| 2022-09-23龙陵MS4.7 | 2022-07-14-2022-07-19 | 90 | 突降超出最低阈值-突升恢复 |
| 2023-05-02隆阳MS5.2 | 无异常 | 30 | 无异常 |
| 2023-12-02芒市MS5.0 | 2023-09-24-2023-10-12 | 147 | 突降超出最低阈值-突升超出阈值高值-突降超出最低阈值 |
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滇西北断裂带痕量氢异常变化及地震对应情况
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| 观测点 | 研究地震 | 异常持续时间 | 震中距/km | 异常特征 |
| 汝南 | 2019-02-02宁蒗MS4.5 | 2019-01-05-2019-02-09 | 85 | 突升超出阈值高值-突降恢复-突升超出阈值高值-波动上升下降 |
| 2019-07-21永胜MS4.8 | 2019-06-24-2019-07-20 | 82 | 突升超出阈值高值-突降恢复-突升超出阈值高值 |
| 2019-11-25洱源MS4.7 | 2019-10-11-2019-10-26 | 102 | 突升超出阈值高值-突降恢复 |
| 2021-05-21漾濞MS6.4 | 无异常 | 115 | 无异常 |
| 2022-01-02宁蒗MS5.5 | 无异常 | 135 | 无异常 |
| 2023-05-02隆阳MS5.2 | 无异常 | 168 | 无异常 |
| 2023-12-02芒市MS5.0 | 2023-08-04-2023-10-20 | 300 | 突升超出阈值高值-突降恢复-突升超出阈值高值-突降恢复、波动幅度大 |
| 洱源 | 2021-05-21漾濞MS6.4 | 2021-02-21-2021-05-08 | 51 | 突降超出阈值低值-持续低值波动-突升恢复-突降超出阈值低值 |
| 2022-01-02宁蒗MS5.5 | 2021-10-18-2022-02-10 | 198 | 突升超出阈值高值-突降恢复-突升超出阈值高值-在高值波动上升下降 |
| 2023-05-02隆阳MS5.2 | 2023-02-08-2023-04-25 | 108 | 趋势下降超出阈值低值-持续低值波动-突升恢复 |
| 2023-12-02芒市MS5.0 | 2023-06-13-2023-06-18 | 279 | 突升超出阈值高值-突降恢复 |
| 弥渡 | 2019-07-21永胜MS4.8 | 2019-04-29-2019-07-23 | 94 | 突升超出阈值高值-持续高值波动-突降恢复-突升超出阈值高值 |
| 2019-11-25洱源MS4.7 | 2019-08-29-2019-11-24 | 99 | 突升超出阈值高值-突降恢复-突升超出阈值高值持续波动 |
| 2021-05-21漾濞MS6.4 | 2021-03-03-2021-03-31 | 68 | 突升超出阈值高值-突降恢复-突升超出阈值高值-突降恢复 |
| 2022-01-02宁蒗MS5.5 | 无异常 | 273 | 无异常 |
| 2023-12-02芒市MS5.0 | 无异常 | 265 | 无异常 |
| 保山 | 2019-11-25洱源MS4.7 | 2019-11-09-2019-11-27 | 106 | 突降超出最低阈值-突升恢复-突降超出最低阈值-突升恢复 |
| 2021-05-13漾濞MS4.6 | 2020-11-20-2021-05-09 | 78 | 突降超出最低阈值-突升恢复、震前数天又多次突升超出阈值高值波动上升下降 |
| 2021-05-21漾濞MS6.4 | 91 |
| 2022-01-02宁蒗MS5.5 | 2021-08-14-2021-12-23 | 300 | 多次突升超出阈值高值-震前数天突升超出阈值-突降恢复 |
| 2022-09-23龙陵MS4.7 | 2022-07-14-2022-07-19 | 90 | 突降超出最低阈值-突升恢复 |
| 2023-05-02隆阳MS5.2 | 无异常 | 30 | 无异常 |
| 2023-12-02芒市MS5.0 | 2023-09-24-2023-10-12 | 147 | 突降超出最低阈值-突升超出阈值高值-突降超出最低阈值 |
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