Article(id=1322566958227238952, tenantId=1146029695717560320, journalId=1281212831689347082, issueId=1322566927927591451, articleNumber=null, orderNo=null, doi=10.14075/j.jgg.2025.04.110, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1743696000000, receivedDateStr=2025-04-04, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1793254134946, onlineDateStr=2026-10-29, pubDate=1773504000000, pubDateStr=2026-03-15, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793254134946, onlineIssueDateStr=2026-10-29, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793254134946, creator=13701087609, updateTime=1793254134946, 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=327, endPage=334, ext={EN=ArticleExt(id=1322566958386622505, articleId=1322566958227238952, tenantId=1146029695717560320, journalId=1281212831689347082, language=EN, title=Segmentation Characteristics of Current Movement of Xianshuihe Fault Zone Based on Deformation Observation, columnId=null, journalTitle=Journal of Geodesy and Geodynamics, columnName=null, runingTitle=null, highlight=null, articleAbstract=
Based on the structural characteristics of the Xianshuihe fault zone, this study divides the five sections of Luhuo, Daofu, Qianning, Zheduotang, and Kangding-Moxi, and quantitatively reveals the horizontal slip rate and kinematic characteristics of each section through multi-source observation data of cross-fault leveling, baseline/ranging, and horizontal creep. The results show that the whole Xianshuihe fault zone is dominated by left-lateral strike-slip mode from 1982 to 2024. The strike-slip rates of Juwo and Xialatuo in Luhuo section are -0.9 mm/a and -2.86 mm/a, and the cumulative strike-slip displacements are 40 mm and 130 mm, which are significantly higher than the activity intensity of Gelu and Xuxu stations. The strike-slip rates of Goupu and Goupu creep stations in Daofu-Qianning section are -0.97 mm/a and -0.58 mm/a, and the cumulative displacement shows a linear growth trend. The horizontal displacement of Longdengba and Laoganning stations is small, and the local fault zone is weakly sinistral. The Zheduotang observation site in the Kangding-Moxi section shows a +0.2 mm/a dextral strike-slip, while the Yulin observation site maintains a stable left-lateral strike-slip of -0.12 mm/a, and its deformation has significant seasonal fluctuations (amplitude of about 1.5 mm to 2.3 mm). The cross-fault leveling of the Anshun site shows continuous tensile normal fault activity, and the linearity of the movement trend reaches 0.933 and 0.824, respectively.The results of segmented comparison show that the activity intensity of the northwestern section is significantly higher than that of the southeastern section, and the vertical movement shows that the thrust of the northern section and the normal fault activity of the southern section are structural inversion. The segmentation difference is related to the fault geometry and the physical properties of the medium. The medium strength of the conversion layer in the northwest section may be lower than that in the southeast section, which is easy to trigger slip and lead to shorter earthquake recurrence period. Combined with the regional stress field, it is found that the locking degree of the Xianshuihe fault zone has changed in different periods, showing that the fault in the northwest section is more active than that in the southeast section, and the locking is weak. At the same time, after the Wenchuan MS8.0 earthquake, the Lushan MS7.0 earthquake, and the Luding MS6.9 earthquake, the extrusion rate of the Bayan Har block to the Sichuan basin accelerated, which affected the far-field left-lateral strike-slip rate of the Xianshuihe fault and the accumulation rate of fault slip deficit, which in turn led to the difference in the stress and strain accumulation rate of each segment on the Xianshuihe fault zone.
, authors=Wen ZHANG
1, Weili WANG
1, Yu LUO
1, Junjun WEN
1, Liyuan PENG
1, Lingli MA
1, Donglin SHU
1, authorsList=Wen ZHANG, Weili WANG, Yu LUO, Junjun WEN, Liyuan PENG, Lingli MA, Donglin SHU, 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=1322566959300980784, articleId=1322566958227238952, tenantId=1146029695717560320, journalId=1281212831689347082, language=CN, title=基于形变观测分析鲜水河断裂带现今运动分段特征, columnId=1281933709121138897, journalTitle=大地测量与地球动力学, columnName=地球动力学, runingTitle=null, highlight=null, articleAbstract=
基于构造特征将鲜水河断裂带划分为炉霍、道孚、乾宁、折多塘、康定-磨西5段，通过跨断层水准、基线/测距及水平蠕变多源观测数据，定量揭示各段水平滑动速率及运动学特征。研究表明，1982—2024年鲜水河断裂带整体以左旋走滑为主导模式，炉霍段侏倭和虾拉沱走滑速率为－0.9 mm/a和－2.86 mm/a，累积走滑量达40 mm和130 mm，显著高于格鲁、虚墟站点活动强度；道孚-乾宁段沟普和沟普蠕变站走滑速率为－0.97 mm/a和－0.58 mm/a，累积位移量呈线性增长趋势；龙灯坝与老乾宁站的水平位移量级较小，局部断裂带呈弱左旋活动。康定-磨西段折多塘观测场地显示+0.2 mm/a的右旋走滑，榆林观测场地则保持－0.12 mm/a的稳定左旋走滑，其形变存在显著季节性波动(振幅约1.5~2.3 mm)，安顺场观测场地跨断层水准测量显示持续张性正断层活动，运动趋势线性度分别达到0.933和0.824。分段对比结果表明，北西段活动强度明显高于南东段，垂直运动表现为北段逆冲与南段正断层活动呈构造反转。分段差异与断层几何结构、介质物理性质有关；北西段转换层介质强度可能低于南东段，易触发滑动，导致较短地震复发周期；结合区域应力场发现，不同时期鲜水河断裂带闭锁程度发生了改变，表现为北西段较南东段断层更为活跃，闭锁较弱。同时，汶川MS8.0、芦山MS7.0及泸定MS6.9地震后，巴颜喀拉地块向四川盆地挤压运动速率加快，影响了鲜水河断裂的远场左旋走滑速率和断层滑动亏损积累速率，进而导致鲜水河断裂带上各分段的应力应变积累速率差异。
, authors=张文
1, 王伟力
1, 罗宇
1, 温军军
1, 彭丽媛
1, 马伶俐
1, 舒东林
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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=RRzHKwR2EVpGC/Sh0xyubw==, magXml=rD/ZvuYNr6wxLuIuDVWdfg==, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=RNDXhr6Mw9Pg2/OXV+BfSg==, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=TQumMbOQdmTLirqMh05CyA==, mapNumber=null, fund=null)}, authors=[Author(id=1322566959611359285, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=1577115002@qq.com, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322566959703633975, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, authorId=1322566959611359285, language=EN, stringName=Wen ZHANG, firstName=Wen, middleName=null, lastName=ZHANG, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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1, address=1 四川省地震局地壳形变观测中心, 雅安, 625000, bio={"content":"
张文, 助理工程师, 主要从事跨断层形变与地震研究, E-mail: 1577115002@qq.com
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张文, 助理工程师, 主要从事跨断层形变与地震研究, E-mail: 1577115002@qq.com
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30 (3): 22- 26, articleTitle=null, refAbstract=null)], funds=[Fund(id=1322566968775913581, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, awardId=LY2516, language=CN, fundingSource=四川省地震局地震科技专项(LY2516), fundOrder=null, country=null), Fund(id=1322566968868188270, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, awardId=LY2420, language=CN, fundingSource=四川省地震局地震科技专项(LY2420), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1322566959510695985, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, xref=null, ext=[AuthorCompanyExt(id=1322566959519084594, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, companyId=1322566959510695985, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=1 Crustal Deformation Monitoring Center of Sichuan Earthquake Agency, Ya'an 625000, China), AuthorCompanyExt(id=1322566959527473203, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, companyId=1322566959510695985, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=1 四川省地震局地壳形变观测中心, 雅安, 625000)])], figs=[ArticleFig(id=1322566967249186913, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=EN, label=Fig. 1, caption=
Near field 3D activity characteristics across faults in the northwest segment of Xianshuihe fault zone, figureFileSmall=oumF8ypa3neVQs+ZDCqjEA==, figureFileBig=RNDXhr6Mw9Pg2/OXV+BfSg==, tableContent=null), ArticleFig(id=1322566967337267298, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=CN, label=图1, caption=
鲜水河断裂带北西段跨断层近场三维活动特征, figureFileSmall=oumF8ypa3neVQs+ZDCqjEA==, figureFileBig=RNDXhr6Mw9Pg2/OXV+BfSg==, tableContent=null), ArticleFig(id=1322566967534399587, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=EN, label=Fig. 2, caption=
Near field 3D activity characteristics across faults in the southeast segment of Xianshuihe fault zone, figureFileSmall=8UJS0AS8/6B7XdMPm8i2Kg==, figureFileBig=eH2z3utDVpzCvC8n1oz4sQ==, tableContent=null), ArticleFig(id=1322566967622479972, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=CN, label=图2, caption=
鲜水河断裂带南东段跨断层近场三维活动特征, figureFileSmall=8UJS0AS8/6B7XdMPm8i2Kg==, figureFileBig=eH2z3utDVpzCvC8n1oz4sQ==, tableContent=null), ArticleFig(id=1322566967702171749, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=EN, label=Fig. 3, caption=
Near field fault activity characteristics of horizontal creep in northwest section of Xianshuihe fault zone, figureFileSmall=dIZrQiz2SFusX0tGdtHdEw==, figureFileBig=1hmdErFA+A+umHe2NRYGxg==, tableContent=null), ArticleFig(id=1322566967857360998, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=CN, label=图3, caption=
鲜水河断裂带北西段水平蠕变近场断层活动特征, figureFileSmall=dIZrQiz2SFusX0tGdtHdEw==, figureFileBig=1hmdErFA+A+umHe2NRYGxg==, tableContent=null), ArticleFig(id=1322566967941247079, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=EN, label=Tab. 1, caption=
Characteristic earthquake rupture sections of Xianshuihe and site layout across faults
, figureFileSmall=null, figureFileBig=null, tableContent=
| 分段 | 序号 | 破裂段名称 | 段长/km | 跨断层观测场地 | 观测手段 | 相邻段重叠量/km | 最近特征地震 |
| 鲜水河 | 1 | 炉霍 | 90 | 侏倭、格鲁、虚墟、虾拉沱
虾拉沱 | 水准、基线/测距
蠕变 | 20 | 1973年MS7.6 |
| 2 | 倡促梁子 | 50 | 恰叫 | 蠕变 | 1923年MS7 1/4 |
| 3 | 道孚 | 45 | 道孚
沟普 | 水准
水准、基线/测距、蠕变 | 10 | 1981年MS6.9 |
| 4 | 松林口-乾宁 | 50 | 龙灯坝、老乾宁 | 水准、基线/测距、蠕变 | 1893年MS7.0 |
| 雅拉河 | 5 | 雅拉河 | 40 | - | - | - | 1700年MS7.0 |
| 色拉哈- 磨西 | 6 | 大炮山 | 45 | - | - | 10 | 1748年MS6.5 |
| 7 | 木格措 | 40 | 榆林 | 水准、基线/测距 | 1725年MS7 1/4 |
| 8 | 磨西 | 80 | 田湾
安顺场 | 水准、基线/测距
水准 | 15 | 2022年MS6.8 |
| 折多塘 | 9 | 折多塘 | 30 | 折多塘 | 水准、基线/测距 | - | 1955年MS7 1/2 |
), ArticleFig(id=1322566968016744552, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=CN, label=表1, caption=
鲜水河特征地震破裂段与跨断层场地布设
, figureFileSmall=null, figureFileBig=null, tableContent=
| 分段 | 序号 | 破裂段名称 | 段长/km | 跨断层观测场地 | 观测手段 | 相邻段重叠量/km | 最近特征地震 |
| 鲜水河 | 1 | 炉霍 | 90 | 侏倭、格鲁、虚墟、虾拉沱
虾拉沱 | 水准、基线/测距
蠕变 | 20 | 1973年MS7.6 |
| 2 | 倡促梁子 | 50 | 恰叫 | 蠕变 | 1923年MS7 1/4 |
| 3 | 道孚 | 45 | 道孚
沟普 | 水准
水准、基线/测距、蠕变 | 10 | 1981年MS6.9 |
| 4 | 松林口-乾宁 | 50 | 龙灯坝、老乾宁 | 水准、基线/测距、蠕变 | 1893年MS7.0 |
| 雅拉河 | 5 | 雅拉河 | 40 | - | - | - | 1700年MS7.0 |
| 色拉哈- 磨西 | 6 | 大炮山 | 45 | - | - | 10 | 1748年MS6.5 |
| 7 | 木格措 | 40 | 榆林 | 水准、基线/测距 | 1725年MS7 1/4 |
| 8 | 磨西 | 80 | 田湾
安顺场 | 水准、基线/测距
水准 | 15 | 2022年MS6.8 |
| 折多塘 | 9 | 折多塘 | 30 | 折多塘 | 水准、基线/测距 | - | 1955年MS7 1/2 |
), ArticleFig(id=1322566968331317353, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=EN, label=Tab. 2, caption=
Basic data of deformation measurement sites across fault in Xianshuihe fault zone
, figureFileSmall=null, figureFileBig=null, tableContent=
| 场地名称 | 斜角直线 | | 直交测线 | 断层产状 |
| 边名 | 夹角/(°) | 边长/m | 边名 | 夹角/(°) | 边长/m |
| 侏倭 | AB | 129.374 | 164.022 | | AC | 40.063 | 283.136 | N45°W/NE∠75°~80° |
| 格蒌 | CA | 129.624 | 96.738 | AB | 81.755 | 72.209 | N40°W/SW∠80° |
| 格鲁 | BA | 147.011 | 117.699 | AC | 59.268 | 151.696 | N55°W/NE∠80° |
| 虚墟 | AB | 139.368 | 227.557 | AC | 52.899 | 244.598 | N40°W/NE∠80° |
| 虾拉沱 | AB | 151.716 | 216.619 | AC | 99.058 | 145.295 | N50°W/NE∠70° |
| 沟普 | AC | 50.728 | 96.502 | AB | 104.549 | 119.604 | N48°W/NE∠60°~80° |
| 龙灯坝 | AB | 129.551 | 74.211 | AD | 33.526 | 68.381 | N45°W/SW∠65° |
| 老乾宁 | G53 | 38.107 | 194.839 | G13 | 74.716 | 172.123 | N35°~45°W/NE∠65°~75° |
| 老乾宁 | BD | 32.014 | 325.418 | AD | 54.901 | 271.971 | N35°~45°W/NE∠65°~75° |
| 虾拉沱蠕变 | 7-3 | 144.659 | 79.334 | 1-3 | 79.611 | 41.180 | N45°~55°W/SE∠60°~80° |
| 恰叫蠕变 | 2-1 | 132.484 | 29.594 | 3-1 | 68.822 | 20.975 | N45°~70°W/SE∠60°~85° |
| 沟普蠕变 | 1-2 | 147.875 | 30.371 | 1-3 | 99.666 | 19.181 | N50°W/NE∠60°W |
| 龙灯坝蠕变 | 1-3 | 39.275 | 26.717 | 1-2 | 98.768 | 20.357 | N36°W/SW∠38° |
| 老乾宁蠕变 | 2-1 | 146.438 | 33.315 | 3-1 | 99.587 | 22.494 | N30°W/NE∠75° |
), ArticleFig(id=1322566968486506602, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=CN, label=表2, caption=
鲜水河断裂带跨断层形变测量场地基础资料
, figureFileSmall=null, figureFileBig=null, tableContent=
| 场地名称 | 斜角直线 | | 直交测线 | 断层产状 |
| 边名 | 夹角/(°) | 边长/m | 边名 | 夹角/(°) | 边长/m |
| 侏倭 | AB | 129.374 | 164.022 | | AC | 40.063 | 283.136 | N45°W/NE∠75°~80° |
| 格蒌 | CA | 129.624 | 96.738 | AB | 81.755 | 72.209 | N40°W/SW∠80° |
| 格鲁 | BA | 147.011 | 117.699 | AC | 59.268 | 151.696 | N55°W/NE∠80° |
| 虚墟 | AB | 139.368 | 227.557 | AC | 52.899 | 244.598 | N40°W/NE∠80° |
| 虾拉沱 | AB | 151.716 | 216.619 | AC | 99.058 | 145.295 | N50°W/NE∠70° |
| 沟普 | AC | 50.728 | 96.502 | AB | 104.549 | 119.604 | N48°W/NE∠60°~80° |
| 龙灯坝 | AB | 129.551 | 74.211 | AD | 33.526 | 68.381 | N45°W/SW∠65° |
| 老乾宁 | G53 | 38.107 | 194.839 | G13 | 74.716 | 172.123 | N35°~45°W/NE∠65°~75° |
| 老乾宁 | BD | 32.014 | 325.418 | AD | 54.901 | 271.971 | N35°~45°W/NE∠65°~75° |
| 虾拉沱蠕变 | 7-3 | 144.659 | 79.334 | 1-3 | 79.611 | 41.180 | N45°~55°W/SE∠60°~80° |
| 恰叫蠕变 | 2-1 | 132.484 | 29.594 | 3-1 | 68.822 | 20.975 | N45°~70°W/SE∠60°~85° |
| 沟普蠕变 | 1-2 | 147.875 | 30.371 | 1-3 | 99.666 | 19.181 | N50°W/NE∠60°W |
| 龙灯坝蠕变 | 1-3 | 39.275 | 26.717 | 1-2 | 98.768 | 20.357 | N36°W/SW∠38° |
| 老乾宁蠕变 | 2-1 | 146.438 | 33.315 | 3-1 | 99.587 | 22.494 | N30°W/NE∠75° |
), ArticleFig(id=1322566968570392683, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=EN, label=Tab. 3, caption=
Movement rate and activity characteristics of five fault segments of Xianshuihe river
, figureFileSmall=null, figureFileBig=null, tableContent=
| 断裂段 | 跨断层场地 | 观测时段 | 活动性质 | 断层走滑速率/mm·a－1 | 断层垂直速率/mm·a－1 |
| 北西段 | 炉霍段 | 侏倭 | 1982—2024年 | 左旋，正断层活动 | －0.90 | +0.63 |
| 格蒌 | 1982—2024年 | 左旋，逆断层活动 | －0.36 | －0.15 |
| 虚墟 | 1982—2024年 | 左旋，逆断层活动 | －0.15 | －0.1 |
| 虾拉沱 | 1989—2024年 | 左旋，逆断层活动 | －2.86 | －0.27 |
| 虾拉沱蠕变 | 1991—2024年 | 左旋 | －0.35 | - |
| 道孚段 | 恰叫蠕变 | 1991—2024年 | 右旋 | +0.09 | - |
| 沟普 | 1984—2024年 | 左旋，逆断层活动 | －0.97 | －0.29 |
| 沟普蠕变 | 1989—2024年 | 左旋 | －0.58 | - |
| 道孚 | 2018—2024年 | 正断层活动 | - | +0.39 |
| 乾宁段 | 龙灯坝 | 1982—2024年 | 左旋，正断层活动 | －0.03 | +0.02 |
| 龙灯坝蠕变 | 1989—2024年 | 左旋 | －0.01 | - |
| 老乾宁 | 1982—2024年 | 左旋，正断层活动 | －0.04 | +0.05 |
| 老乾宁蠕变 | 1990—2024年 | 左旋 | －0.06 | - |
| 南东段 | 色拉哈-磨西段 | 榆林 | 2018—2024年 | 左旋，正断层活动 | －0.12 | +0.07 |
| 安顺场 | 1978—2024年 | 正断层活动 | - | +0.26 |
| 折多塘段 | 折多塘 | 1985—2024年 | 右旋，逆断层活动 | +0.2 | －0.02 |
), ArticleFig(id=1322566968683638892, tenantId=1146029695717560320, journalId=1281212831689347082, articleId=1322566958227238952, language=CN, label=表3, caption=
鲜水河5个断裂段运动速率及活动性质
, figureFileSmall=null, figureFileBig=null, tableContent=
| 断裂段 | 跨断层场地 | 观测时段 | 活动性质 | 断层走滑速率/mm·a－1 | 断层垂直速率/mm·a－1 |
| 北西段 | 炉霍段 | 侏倭 | 1982—2024年 | 左旋，正断层活动 | －0.90 | +0.63 |
| 格蒌 | 1982—2024年 | 左旋，逆断层活动 | －0.36 | －0.15 |
| 虚墟 | 1982—2024年 | 左旋，逆断层活动 | －0.15 | －0.1 |
| 虾拉沱 | 1989—2024年 | 左旋，逆断层活动 | －2.86 | －0.27 |
| 虾拉沱蠕变 | 1991—2024年 | 左旋 | －0.35 | - |
| 道孚段 | 恰叫蠕变 | 1991—2024年 | 右旋 | +0.09 | - |
| 沟普 | 1984—2024年 | 左旋，逆断层活动 | －0.97 | －0.29 |
| 沟普蠕变 | 1989—2024年 | 左旋 | －0.58 | - |
| 道孚 | 2018—2024年 | 正断层活动 | - | +0.39 |
| 乾宁段 | 龙灯坝 | 1982—2024年 | 左旋，正断层活动 | －0.03 | +0.02 |
| 龙灯坝蠕变 | 1989—2024年 | 左旋 | －0.01 | - |
| 老乾宁 | 1982—2024年 | 左旋，正断层活动 | －0.04 | +0.05 |
| 老乾宁蠕变 | 1990—2024年 | 左旋 | －0.06 | - |
| 南东段 | 色拉哈-磨西段 | 榆林 | 2018—2024年 | 左旋，正断层活动 | －0.12 | +0.07 |
| 安顺场 | 1978—2024年 | 正断层活动 | - | +0.26 |
| 折多塘段 | 折多塘 | 1985—2024年 | 右旋，逆断层活动 | +0.2 | －0.02 |
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