Article(id=1322566994793181453, tenantId=1146029695717560320, journalId=1281212831689347082, issueId=1322566927927591451, articleNumber=null, orderNo=null, doi=10.14075/j.jgg.2025.03.102, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1743004800000, receivedDateStr=2025-03-27, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1793254143664, onlineDateStr=2026-10-29, pubDate=1773504000000, pubDateStr=2026-03-15, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793254143664, onlineIssueDateStr=2026-10-29, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793254143664, creator=13701087609, updateTime=1793254143664, updator=13701087609, issue=Issue{id=1322566927927591451, tenantId=1146029695717560320, journalId=1281212831689347082, year='2026', volume='46', issue='3', pageStart='262', pageEnd='391', issueExtLink='null', onlineDate='null', pubDate='1773504000000', pubDateStr='2026-03-15', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1793254127723, creator='13701087609', updateTime=1793254127723, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=343, endPage=348, ext={EN=ArticleExt(id=1322566994965147918, articleId=1322566994793181453, tenantId=1146029695717560320, journalId=1281212831689347082, language=EN, title=Verification and Analysis of the Dashuitou Cross-Fault Site, Haiyuan Fault, Based on InSAR Technology, columnId=null, journalTitle=Journal of Geodesy and Geodynamics, columnName=null, runingTitle=null, highlight=null, articleAbstract=

The observed data show that the BM1-BM3 branch of the Dashuitou cross-fault in the Haiyuan fault zone exhibited a reverse faulting change of 1.52 mm in November 2023, and another sudden reverse faulting jump of 1.71 mm on March 6, 2024. To verify whether this anomaly is related to tectonic movement, we obtain the time series of surface deformation in the Dashuitou cross-fault site by InSAR technology. It analyzes the possible causes of the cross-fault deformation anomaly from the deformation field's spatial distribution and time evolution. The results show that: 1) The coal mining areas around the site have obvious subsidence, and the subsidence rate changes rapidly over time. The cumulative shape variable from January 2023 to June 2024 is about 23 cm, and the significant deformation range is about 1 km². 2) The benchmark points are significantly affected by mining-induced subsidence, exhibiting varying degrees of settlement over time. The closer they are to the mining area, the greater the subsidence magnitude and the faster the rate. 3) Comparing the results of InSAR and leveling observation, the trend and magnitude of cross-fault deformation in the same period are the same. In summary, the abnormal leveling deformation of the Dashuitou cross-fault site may be caused by the settlement of the mining area.

, authors=Yanhui LIU¹, Lingyun JI^1, *, Liangyu ZHU¹, Chuanjin LIU¹, Wenting ZHANG¹, authorsList=Yanhui LIU, Lingyun JI, Liangyu ZHU, Chuanjin LIU, Wenting ZHANG, authorCompany=null, correspAuthors=Lingyun JI, 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=1322566998689689889, articleId=1322566994793181453, tenantId=1146029695717560320, journalId=1281212831689347082, language=CN, title=基于InSAR技术的海原断裂大水头跨断层场地异常核实与分析, columnId=1322566785874908034, journalTitle=大地测量与地球动力学, columnName=特色栏目: 地震大地测量学, runingTitle=null, highlight=null, articleAbstract=

观测资料显示，海原断裂带大水头跨断层BM1-BM3支线于2023-11出现1.52 mm的逆断变化，2024-03-06再次出现1.71 mm的逆断突跳变化。为核实此次异常是否与构造运动有关，利用InSAR技术获取大水头跨断层场地区域地表形变的时间序列，从形变场空间展布以及时间演化2个方面，分析跨断层形变异常的可能成因。结果表明：1)场地周围的煤矿开采区沉降明显，且沉降速率随时间变化较快，2023-01—2024-06的累积沉降量最大约23 cm，显著沉降范围最大约1 km²；2)水准点受矿区沉降影响显著，且随时间的推移均有不同程度的沉降，距离矿区越近沉降量级越大，速率越快；3)对比InSAR与水准观测结果，发现同时间段跨断层形变趋势和量级基本一致。综上，大水头跨断层水准形变异常极大可能是矿区沉降导致的。

, authors=刘艳慧¹, 季灵运^1, *, 朱良玉¹, 刘传金¹, 张文婷¹, authorsList=刘艳慧, 季灵运, 朱良玉, 刘传金, 张文婷, authorCompany=null, correspAuthors=季灵运, authorNote=, correspAuthorsNote=, 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=5ZteV+x8AZAPrb09Oj8PQw==, magXml=/WjvrLy9DFwTI3SzPwJLIw==, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=y2pnWQuBU5PITH7HPvHcHg==, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=wWfjNU6QYYMJbO3rhzZHKg==, mapNumber=null, fund=null)}, authors=[Author(id=1322566998991679782, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566994793181453, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=2513178156@qq.com, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322566999062982952, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566994793181453, authorId=1322566998991679782, language=EN, stringName=Yanhui LIU, firstName=Yanhui, middleName=null, lastName=LIU, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=1 The Second Monitoring and Application Center, CEA, Xi'an 710054, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1322566999138480425, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566994793181453, authorId=1322566998991679782, language=CN, stringName=刘艳慧, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=1 中国地震局第二监测中心, 西安, 710054, bio={"content":"

刘艳慧, 工程师, 主要从事大地测量资料应用分析, E-mail: 2513178156@qq.com

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刘艳慧, 工程师, 主要从事大地测量资料应用分析, E-mail: 2513178156@qq.com

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紫色编号的十字表示参与计算的影像，红色编号的十字表示未参与计算的影像，紫色直线表示生成的干涉图

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黑色矩形表示深度，灰色圆圈表示体积

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