Article(id=1322940816418812272, tenantId=1146029695717560320, journalId=1281212831689347082, issueId=1322940717152215106, articleNumber=null, orderNo=null, doi=10.14075/j.jgg.2024.05.209, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1715011200000, receivedDateStr=2024-05-07, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1793343269686, onlineDateStr=2026-10-30, pubDate=1744646400000, pubDateStr=2025-04-15, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793343269686, onlineIssueDateStr=2026-10-30, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793343269686, creator=13701087609, updateTime=1793343269686, updator=13701087609, issue=Issue{id=1322940717152215106, tenantId=1146029695717560320, journalId=1281212831689347082, year='2025', volume='45', issue='4', pageStart='331', pageEnd='440', issueExtLink='null', onlineDate='null', pubDate='1744646400000', pubDateStr='2025-04-15', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1793343246019, creator='13701087609', updateTime=1793343246019, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=426, endPage=430, 435, ext={EN=ArticleExt(id=1322940816624333169, articleId=1322940816418812272, tenantId=1146029695717560320, journalId=1281212831689347082, language=EN, title=Vertical Movement Characteristics of the Northern Margin Fault of Western Qinling Mountains Using Precise Leveling Data, columnId=null, journalTitle=Journal of Geodesy and Geodynamics, columnName=null, runingTitle=null, highlight=null, articleAbstract=

Using precise leveling measurement data and a modified dip-slip displacement model, we systematic analyze the vertical movement characteristics of each section of the northern margin fault of western Qinling mountains. The results show that the northern margin fault of western Qinling mountains is undergoing a composite deformation mechanism of left-lateral strike-slip and thrust compression, and the activity varies among different sections. The vertical dip-slip rate increase from 0.24 mm/a in the western section to a maximum of 2.31 mm/a in the eastern section, and then decrease to 1.51 mm/a. The inverted locking depths are consistent with the relocation depths of small earthquakes, which indicates that there are different locking states in each section. Combining seismic activity, the Tianshui-Baoji section has the highest earthquake risk.

, authors=Bo ZHAO¹, Lingyun JI¹, Ming HAO¹, Jiangtao QIU¹, Liangyu ZHU¹, Fengyun JIANG¹, Lei LIU¹, authorsList=Bo ZHAO, Lingyun JI, Ming HAO, Jiangtao QIU, Liangyu ZHU, Fengyun JIANG, Lei LIU, authorCompany=null, correspAuthors=null, authorNote=, 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=1322940819438711164, articleId=1322940816418812272, tenantId=1146029695717560320, journalId=1281212831689347082, language=CN, title=利用精密水准资料研究西秦岭北缘断裂带的垂向运动特征, columnId=1322506197874356701, journalTitle=大地测量与地球动力学, columnName=地壳运动, runingTitle=null, highlight=null, articleAbstract=

利用精密水准测量数据，结合改进的倾滑位移模型，系统分析西秦岭北缘断裂带各区段的垂向运动特征。结果表明，西秦岭北缘断裂带正经历左旋走滑与逆冲挤压的复合变形机制，且不同区段的活动性存在显著差异。垂向倾滑速率呈现从西段的0.24 mm/a向东增大到2.31 mm/a后，又减小到1.51 mm/a的空间变化趋势。通过反演获得的闭锁深度与地震精定位所揭示的小震活动深度高度吻合，说明该断裂带各区段处于不同的闭锁状态。结合地震活动性发现，天水-宝鸡段发震危险性最紧迫。

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ZHAO Bo, engineer, majors in geodesy, E-mail: 554893513@qq.com

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赵勃, 工程师, 主要从事大地测量研究, E-mail: 554893513@qq.com

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赵勃, 工程师, 主要从事大地测量研究, E-mail: 554893513@qq.com

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(a)~(e)中红线为拟合的速率曲线，位置见图1；(f)中红色虚线为反演的闭锁深度，小震重新定位目录由中国地震局地球物理研究所房立华研究员提供，时间跨度为1970—2012年

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The dip rate of faults obtained by leveling data

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断裂区域	走向/(°)	倾角/(°)	闭锁深度/ km	倾滑速率/mm·a-1
锅麻滩段(a)	N75°W	49	8.1	0.24
漳县段(b)	N69°W	48	25.2	-0.86
鸳凤段(c)	N71°W	60	32.5	2.31
天水-宝鸡段(d)	N79°W	49	21.8	1.51
天水-宝鸡段(e)	N79°W	51	12.2	-1.19

), ArticleFig(id=1322940824773865910, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322940816418812272, language=CN, label=表1, caption=

水准数据反演的断裂区域倾滑速率结果

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断裂区域	走向/(°)	倾角/(°)	闭锁深度/ km	倾滑速率/mm·a-1
锅麻滩段(a)	N75°W	49	8.1	0.24
漳县段(b)	N69°W	48	25.2	-0.86
鸳凤段(c)	N71°W	60	32.5	2.31
天水-宝鸡段(d)	N79°W	49	21.8	1.51
天水-宝鸡段(e)	N79°W	51	12.2	-1.19

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