Article(id=1311999380052336675, tenantId=1146029695717560320, journalId=1311385891987619962, issueId=1311998530802250506, articleNumber=null, orderNo=null, doi=10.12090/j.issn.1006-6616.2025039, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1744128000000, receivedDateStr=2025-04-09, revisedDate=1761494400000, revisedDateStr=2025-10-27, acceptedDate=1763913600000, acceptedDateStr=2025-11-24, onlineDate=1790734627974, onlineDateStr=2026-09-30, pubDate=1787846400000, pubDateStr=2026-08-28, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1790734627974, onlineIssueDateStr=2026-09-30, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1790734627974, creator=13701087609, updateTime=1790734627974, updator=13701087609, issue=Issue{id=1311998530802250506, tenantId=1146029695717560320, journalId=1311385891987619962, year='2026', volume='32', issue='4', pageStart='771', pageEnd='998', issueExtLink='null', onlineDate='null', pubDate='1787846400000', pubDateStr='2026-08-28', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=1, specialIssue=null, createTime=1790734425497, creator='13701087609', updateTime=1790739498146, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1312019807097160415, tenantId=1146029695717560320, journalId=1311385891987619962, issueId=1311998530802250506, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1312019807097160416, tenantId=1146029695717560320, journalId=1311385891987619962, issueId=1311998530802250506, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=806, endPage=816, ext={EN=ArticleExt(id=1311999380450795556, articleId=1311999380052336675, tenantId=1146029695717560320, journalId=1311385891987619962, language=EN, title=Fractal characteristics of karst geology in large-scale thrust-nappe tectonic settings, columnId=1311998890077938361, journalTitle=Journal of Geomechanics, columnName=Tectonic System & Structural Geology, runingTitle=null, highlight=null, articleAbstract=
Objective Large-scale thrust-nappe structures have a significant impact on the regional geological environment and are important factors controlling the development of karst systems. Quantitative analysis of karst geological fractal characteristics in such settings provides essential scientific insights into the nonlinear behavior of complex karst systems.
Methods Focusing on the karst region along the Qingfeng fault zone, the box-counting dimension method of geological fractal theory was used to quantify key geological elements. We evaluated the fractal characteristics across both regional scales and watershed units to determine their fractal dimensions and scaling properties.
Results The stratigraphic boundaries at both regional and watershed scales exhibit pronounced fractal characteristics. Karstification significantly enhances boundary complexity, leading to higher fractal dimensions in areas with more advanced karst development. Furthermore, thrust-nappe structures and tectonic movements strongly influence drainage network fractals, modifying the conventional spatial mapping between surface and groundwater systems. The fractal dimensions of surface drainage systems show a positive correlation with those of subsurface karst drainage systems. Peak landforms in the study area exhibit youth-stage peak-cluster characteristics, indicating an early stage in the regional karst geomorphic cycle.
Conclusions Karst in the region exhibits fractal characteristics, and the peak evolution follows the three-stage patterns common in karst areas. Surface and groundwater systems have positively correlated fractal patterns, and stratigraphic boundary dimensions serve as a robust indicator of karst development intensity.
Significance Clarifying the self-similarity of karst in thrust-nappe tectonic zones provides a quantitative reference and theoretical basis for assessing the relationships between faulting, karst distribution, and evolutionary dynamics, offering a valuable methodological approach for addressing similar karst geological issues.
, authors=Xiaodi SHI, Jianxin YAO, Biyi ZHAO, Dan YAO, Li KUANG, authorsList=Xiaodi SHI, Jianxin YAO, Biyi ZHAO, Dan YAO, Li KUANG, authorCompany=null, correspAuthors=Jianxin YAO, authorNote=null, correspAuthorsNote=null, copyrightStatement=Copyright ©2026 Journal of Geomechanics. All rights reserved., 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=1311999393415389264, articleId=1311999380052336675, tenantId=1146029695717560320, journalId=1311385891987619962, language=CN, title=大型逆冲推覆构造地质背景下喀斯特地质分形特征, columnId=1311998893139780288, journalTitle=地质力学学报, columnName=构造体系与构造地质, runingTitle=null, highlight=null, articleAbstract=
大型逆冲推覆构造对区域地质环境具有显著影响，是控制喀斯特体系发育的重要因素。探究在此背景下的喀斯特地质分形特征，能够为分析复杂喀斯特系统非线性问题提供科学依据。以青峰大断裂喀斯特区为研究对象，采用地质分形理论盒维数法量化区内各典型要素，探讨区域要素及流域单元要素分形特征，确定各典型要素分维值及分形特征。研究结果表明：区域和流域单元地层线均具有明显分形特征，喀斯特化进程对地层线具有明显的增维作用，喀斯特越发育，分维值越大；同时逆冲推覆构造及构造运动对水系分形特征影响较大，会改变地表水系与地下水系的一般映射关系，地表水系分维值与地下喀斯特水系统分维值呈现近似正相关规律。青峰断裂带喀斯特区峰体表现为幼年期峰丛地貌，表明其现处于喀斯特旋回发育的早期。区内喀斯特具有分形特征，峰体演化遵循一般喀斯特区的三段式演化规律，地表水系与地下水系表现出正相关的分形规律，地层线分维值对喀斯特发育程度具有明显的指示意义。明确逆冲推覆构造区的喀斯特自相似性，可为研究断裂构造与喀斯特分布、发育程度及演化规律提供定量化分析的参考和理论依据，也为解决同类地区中喀斯特地质问题提供了新思路。
, authors=史箫笛, 姚建新, 赵碧义, 姚丹, 况丽, authorsList=史箫笛, 姚建新, 赵碧义, 姚丹, 况丽, authorCompany=null, correspAuthors=姚建新, authorNote=
作者贡献声明
史箫笛、姚建新负责论文构思、数据分析、研究方法和论文写作；史箫笛、姚建新、赵碧义参与数据分析和技术手段的实践应用和绘图；史箫笛、姚丹、况丽参与数据分析、研究方法和修改。所有作者均阅读并同意稿件的提交和发表。
Author’s Contributions
SHI Xiaodi and YAO Jianxin conceived the study, performed data analysis, designed the research methodology, and drafted the manuscript; SHI Xiaodi, YAO Jianxin, and ZHAO Biyi participated in data analysis, practical application of technical approaches, and figure generation; SHI Xiaodi, YAO Dan and KUANG Li were involved in data analysis, refinement of the research methodology, and manuscript revision. All authors have read and approved the submission and publication of the manuscript.
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unstructuredReference=张满仓, 兰天伟, 贾伟东, 等, 2023. 断裂构造分形几何特征对冲击地压的控制作用研究[J]. 煤炭工程, 55(5): 103-110., articleTitle=null, refAbstract=null), Reference(id=1311999438239916266, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, doi=null, pmid=null, pmcid=null, year=null, volume=null, issue=null, pageStart=null, pageEnd=null, url=null, language=null, rfNumber=79, rfOrder=78, authorNames=null, journalName=null, refType=null, unstructuredReference=张元, 王红岩, 李育, 等, 2024. 西秦岭夏河-合作地区断裂构造分形结构特征及成矿预测[J]. 矿床地质, 43(2): 359-372., articleTitle=null, refAbstract=null), Reference(id=1311999438332190955, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, doi=null, pmid=null, pmcid=null, year=null, volume=null, issue=null, pageStart=null, pageEnd=null, url=null, language=null, rfNumber=80, rfOrder=79, authorNames=null, journalName=null, refType=null, unstructuredReference=赵海军, 张家祥, 彭昊, 等, 2025. 考虑参数不确定性的强震区危岩崩塌运动规律分析[J]. 工程地质学报, 33(1): 224-239., articleTitle=null, refAbstract=null), Reference(id=1311999438659346668, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, doi=null, pmid=null, pmcid=null, year=null, volume=null, issue=null, pageStart=null, pageEnd=null, url=null, language=null, rfNumber=81, rfOrder=80, authorNames=null, journalName=null, refType=null, unstructuredReference=周宁, 刘波, 2009. 鄂西南岩溶地区表层岩溶带发育强度变化规律研究[J]. 中国岩溶, 28(1): 1-6., articleTitle=null, refAbstract=null), Reference(id=1311999438730649837, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, doi=null, pmid=null, pmcid=null, year=null, volume=null, issue=null, pageStart=null, pageEnd=null, url=null, language=null, rfNumber=82, rfOrder=81, authorNames=null, journalName=null, refType=null, unstructuredReference=朱晓华, 王建, 陆娟, 2001. 关于地学中分形理论应用的思考[J]. 南京师大学报(自然科学版), 24(3): 93-98., articleTitle=null, refAbstract=null), Reference(id=1311999438793564398, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, doi=null, pmid=null, pmcid=null, year=null, volume=null, issue=null, pageStart=null, pageEnd=null, url=null, language=null, rfNumber=83, rfOrder=82, authorNames=null, journalName=null, refType=null, unstructuredReference=朱晓华, 蔡运龙, 2003. 中国水系的盒维数及其关系[J]. 水科学进展, 14(6): 731-735., articleTitle=null, refAbstract=null), Reference(id=1311999439078777071, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, doi=null, pmid=null, pmcid=null, year=null, volume=null, issue=null, pageStart=null, pageEnd=null, url=null, language=null, rfNumber=84, rfOrder=83, authorNames=null, journalName=null, refType=null, unstructuredReference=邹明清, 2007. 分形理论的若干应用[D]. 武汉: 华中科技大学., articleTitle=null, refAbstract=null)], funds=null, companyList=[AuthorCompany(id=1311999396053606482, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, xref=null, 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Structural and geological maps of central Fengxi Town, figureFileSmall=14VOQEZCDUIwB28A76QStA==, figureFileBig=u2RN56T9dAO4BeC67oq4sA==, tableContent=null), ArticleFig(id=1311999408481329277, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=图1, caption=
丰溪镇中部地区构造及地质简图, figureFileSmall=14VOQEZCDUIwB28A76QStA==, figureFileBig=u2RN56T9dAO4BeC67oq4sA==, tableContent=null), ArticleFig(id=1311999410570092670, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=EN, label=Fig.2, caption=
Karst landform zonation map of central Fengxi Town, figureFileSmall=KiXgVrjgwzUSqUQMPGncww==, figureFileBig=AcPtle2AI9Z9Bgdl0ST5pQ==, tableContent=null), ArticleFig(id=1311999410691727487, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=图2, caption=
丰溪镇中部地区喀斯特地貌分区图, figureFileSmall=KiXgVrjgwzUSqUQMPGncww==, figureFileBig=AcPtle2AI9Z9Bgdl0ST5pQ==, tableContent=null), ArticleFig(id=1311999411081797760, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=EN, label=Fig.3, caption=
Linear regression fit for the Gaozu River drainage system, figureFileSmall=UtWYRjf1JvdQgDbSxTd5AA==, figureFileBig=NA2eDk8wEAL5Ue16ENN5tw==, tableContent=null), ArticleFig(id=1311999411492839553, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=图3, caption=
水系（高祖河）线性回归曲线r—网格边长；$ N\left(r\right) $—盒子数
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Watershed unit zonation map, figureFileSmall=S7J6N/d9X3E3YH+EmmKvfw==, figureFileBig=doAkVhsj0/pjiEyxFo18Pw==, tableContent=null), ArticleFig(id=1311999412319117443, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=图4, caption=
流域单元分区图, figureFileSmall=S7J6N/d9X3E3YH+EmmKvfw==, figureFileBig=doAkVhsj0/pjiEyxFo18Pw==, tableContent=null), ArticleFig(id=1311999412675633284, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=EN, label=Fig.5, caption=
Schematic diagram of peak evolution stages, figureFileSmall=mBMAmryEOGkwcAKdnZvzEw==, figureFileBig=GHLFR4C4qmeY3gaEACJTjg==, tableContent=null), ArticleFig(id=1311999412826628229, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=图5, caption=
峰体演化阶段示意图a—喀斯特化阶段与峰体形态示意图；b—喀斯特化阶段峰体曲线示意图
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Peak profile characteristic curves of central Fengxi Town, figureFileSmall=z9SoC4nk1cO2OoDqkH1D1A==, figureFileBig=OhumgaxnF4de20TphXpO1w==, tableContent=null), ArticleFig(id=1311999415175438473, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=图6, caption=
丰溪镇中部地区峰体特征曲线, figureFileSmall=z9SoC4nk1cO2OoDqkH1D1A==, figureFileBig=OhumgaxnF4de20TphXpO1w==, tableContent=null), ArticleFig(id=1311999415292878986, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=EN, label=Tab.1, caption=
Fractal grid counts of the Gaozu River drainage system
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| 方形网边长r | 网格数$ N\left(r\right) $ | $ \lg r $ | $ \lg N\left(r\right) $ |
| 500 m | 19 | 2.6990 | 1.2788 |
| 300 m | 34 | 2.4771 | 1.5315 |
| 200 m | 50 | 2.3010 | 1.6990 |
| 150 m | 67 | 2.1761 | 1.8261 |
| 100 m | 103 | 2.0000 | 2.0128 |
| 80 m | 131 | 1.9031 | 2.1173 |
| 50 m | 209 | 1.6990 | 2.3201 |
| 30 m | 350 | 1.4771 | 2.5441 |
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水系（高祖河）分形网格数
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| 方形网边长r | 网格数$ N\left(r\right) $ | $ \lg r $ | $ \lg N\left(r\right) $ |
| 500 m | 19 | 2.6990 | 1.2788 |
| 300 m | 34 | 2.4771 | 1.5315 |
| 200 m | 50 | 2.3010 | 1.6990 |
| 150 m | 67 | 2.1761 | 1.8261 |
| 100 m | 103 | 2.0000 | 2.0128 |
| 80 m | 131 | 1.9031 | 2.1173 |
| 50 m | 209 | 1.6990 | 2.3201 |
| 30 m | 350 | 1.4771 | 2.5441 |
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Fractal characteristics of regional drainage systems
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方形网
边长（r）/m | 500 | 300 | 200 | 150 | 100 | 80 | 50 | 30 | 分维值 |
| 水系名称 | 网格数$ N\left(r\right) $ |
| 高祖河 | 19 | 34 | 50 | 67 | 103 | 131 | 209 | 350 | 1.0311 |
| 泉河 | 38 | 72 | 106 | 143 | 221 | 287 | 446 | 739 | 1.0473 |
| 石甸河 | 8 | 14 | 22 | 28 | 42 | 50 | 85 | 134 | 0.9956 |
| 五石道河 | 3 | 4 | 5 | 6 | 9 | 11 | 19 | 30 | 0.8382 |
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区域水系分形特征
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方形网
边长（r）/m | 500 | 300 | 200 | 150 | 100 | 80 | 50 | 30 | 分维值 |
| 水系名称 | 网格数$ N\left(r\right) $ |
| 高祖河 | 19 | 34 | 50 | 67 | 103 | 131 | 209 | 350 | 1.0311 |
| 泉河 | 38 | 72 | 106 | 143 | 221 | 287 | 446 | 739 | 1.0473 |
| 石甸河 | 8 | 14 | 22 | 28 | 42 | 50 | 85 | 134 | 0.9956 |
| 五石道河 | 3 | 4 | 5 | 6 | 9 | 11 | 19 | 30 | 0.8382 |
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Fractal characteristics of regional stratigraphic boundaries
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| 地层代号 | 喀斯特层组 | 方形网边长（r）/m | 500 | 300 | 200 | 150 | 100 | 80 | 50 | 30 | 分维值 | 喀斯特发育程度 |
| 岩性 | 网格数N(r) |
| Є2qn | 夹层状碳酸盐岩 | 泥质白云岩 | 10 | 15 | 22 | 29 | 43 | 52 | 83 | 138 | 0.9399 | 弱 |
| Є1t | 夹层状碳酸盐岩 | 灰岩 | 11 | 15 | 20 | 28 | 43 | 55 | 89 | 149 | 0.9589 | 弱 |
| Є1sl | 纯层碳酸盐岩 | 灰岩 | 119 | 222 | 352 | 472 | 706 | 882 | 1410 | 2350 | 1.0475 | 强 |
| Є1s | 间互状碳酸盐岩 | 灰岩 | 90 | 151 | 231 | 316 | 476 | 597 | 953 | 1591 | 1.0137 | 中等 |
| Z2dn | 纯层碳酸盐岩 | 白云岩 | 43 | 60 | 93 | 123 | 184 | 231 | 366 | 609 | 1.0242 | 强 |
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区域地层线分形特征
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| 地层代号 | 喀斯特层组 | 方形网边长（r）/m | 500 | 300 | 200 | 150 | 100 | 80 | 50 | 30 | 分维值 | 喀斯特发育程度 |
| 岩性 | 网格数N(r) |
| Є2qn | 夹层状碳酸盐岩 | 泥质白云岩 | 10 | 15 | 22 | 29 | 43 | 52 | 83 | 138 | 0.9399 | 弱 |
| Є1t | 夹层状碳酸盐岩 | 灰岩 | 11 | 15 | 20 | 28 | 43 | 55 | 89 | 149 | 0.9589 | 弱 |
| Є1sl | 纯层碳酸盐岩 | 灰岩 | 119 | 222 | 352 | 472 | 706 | 882 | 1410 | 2350 | 1.0475 | 强 |
| Є1s | 间互状碳酸盐岩 | 灰岩 | 90 | 151 | 231 | 316 | 476 | 597 | 953 | 1591 | 1.0137 | 中等 |
| Z2dn | 纯层碳酸盐岩 | 白云岩 | 43 | 60 | 93 | 123 | 184 | 231 | 366 | 609 | 1.0242 | 强 |
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Fractal characteristics of stratigraphic boundaries in watershed units
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| 单元编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 |
| “/”表示该单元内无地层线 |
| 1 | 0.8523 | 16 | / | 31 | / | 46 | 1.0115 | 61 | 0.7553 | 76 | 0.8496 | 91 | 0.7503 |
| 2 | 0.8814 | 17 | / | 32 | 0.7664 | 47 | 0.8873 | 62 | 0.8506 | 77 | | 92 | 0.7583 |
| 3 | 0.9111 | 18 | 0.8437 | 33 | 0.9520 | 48 | 0.8379 | 63 | / | 78 | 0.9170 | 93 | / |
| 4 | / | 19 | / | 34 | 0.8613 | 49 | / | 64 | 0.8916 | 79 | 0.8753 | 94 | 0.8836 |
| 5 | / | 20 | / | 35 | 0.9220 | 50 | / | 65 | / | 80 | 0.8889 | 95 | / |
| 6 | 0.8834 | 21 | / | 36 | / | 51 | 0.8726 | 66 | 0.9040 | 81 | 1.0267 | 96 | / |
| 7 | / | 22 | 0.9220 | 37 | 0.9329 | 52 | 0.8814 | 67 | 0.8287 | 82 | 0.8922 | 97 | 0.9018 |
| 8 | 0.9379 | 23 | / | 38 | / | 53 | 0.7356 | 68 | 0.9450 | 83 | 0.7805 | 98 | / |
| 9 | / | 24 | / | 39 | / | 54 | 0.8344 | 69 | / | 84 | 0.9225 | 99 | 0.8691 |
| 10 | 0.9144 | 25 | 0.9502 | 40 | 0.8646 | 55 | 0.9127 | 70 | / | 85 | 0.9992 | 100 | / |
| 11 | / | 26 | / | 41 | 0.9161 | 56 | 0.9401 | 71 | / | 86 | / | 101 | 0.8053 |
| 12 | / | 27 | 0.9174 | 42 | / | 57 | 0.7369 | 72 | 0.9085 | 87 | / | 102 | 0.7801 |
| 13 | / | 28 | 0.8994 | 43 | 0.9149 | 58 | 0.8287 | 73 | 0.9776 | 88 | 0.8860 | 103 | / |
| 14 | 0.9825 | 29 | 0.9613 | 44 | 0.8414 | 59 | 0.7533 | 74 | 0.8836 | 89 | / | | |
| 15 | 0.7342 | 30 | / | 45 | / | 60 | 0.7426 | 75 | 0.8048 | 90 | 1.0814 | | |
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流域单元地层线分形特征
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| 单元编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 | 单元
编号 | 分维值 |
| “/”表示该单元内无地层线 |
| 1 | 0.8523 | 16 | / | 31 | / | 46 | 1.0115 | 61 | 0.7553 | 76 | 0.8496 | 91 | 0.7503 |
| 2 | 0.8814 | 17 | / | 32 | 0.7664 | 47 | 0.8873 | 62 | 0.8506 | 77 | | 92 | 0.7583 |
| 3 | 0.9111 | 18 | 0.8437 | 33 | 0.9520 | 48 | 0.8379 | 63 | / | 78 | 0.9170 | 93 | / |
| 4 | / | 19 | / | 34 | 0.8613 | 49 | / | 64 | 0.8916 | 79 | 0.8753 | 94 | 0.8836 |
| 5 | / | 20 | / | 35 | 0.9220 | 50 | / | 65 | / | 80 | 0.8889 | 95 | / |
| 6 | 0.8834 | 21 | / | 36 | / | 51 | 0.8726 | 66 | 0.9040 | 81 | 1.0267 | 96 | / |
| 7 | / | 22 | 0.9220 | 37 | 0.9329 | 52 | 0.8814 | 67 | 0.8287 | 82 | 0.8922 | 97 | 0.9018 |
| 8 | 0.9379 | 23 | / | 38 | / | 53 | 0.7356 | 68 | 0.9450 | 83 | 0.7805 | 98 | / |
| 9 | / | 24 | / | 39 | / | 54 | 0.8344 | 69 | / | 84 | 0.9225 | 99 | 0.8691 |
| 10 | 0.9144 | 25 | 0.9502 | 40 | 0.8646 | 55 | 0.9127 | 70 | / | 85 | 0.9992 | 100 | / |
| 11 | / | 26 | / | 41 | 0.9161 | 56 | 0.9401 | 71 | / | 86 | / | 101 | 0.8053 |
| 12 | / | 27 | 0.9174 | 42 | / | 57 | 0.7369 | 72 | 0.9085 | 87 | / | 102 | 0.7801 |
| 13 | / | 28 | 0.8994 | 43 | 0.9149 | 58 | 0.8287 | 73 | 0.9776 | 88 | 0.8860 | 103 | / |
| 14 | 0.9825 | 29 | 0.9613 | 44 | 0.8414 | 59 | 0.7533 | 74 | 0.8836 | 89 | / | | |
| 15 | 0.7342 | 30 | / | 45 | / | 60 | 0.7426 | 75 | 0.8048 | 90 | 1.0814 | | |
), ArticleFig(id=1311999417863987346, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=EN, label=Tab.5, caption=
Fractal characteristics of stratigraphic boundaries in regional watershed units
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| 级次 | 分形特征 | 地层代号 |
| Є2qn | Є1t | Є1sl | Є1s | Z2dn |
| 流域单元 | 分维值 | 0.8170 | 0.8589 | 0.9008 | 0.8607 | 0.8954 |
| 区域单元 | 0.9399 | 0.9589 | 1.0475 | 1.0137 | 1.0242 |
), ArticleFig(id=1311999419482988691, tenantId=1146029695717560320, journalId=1311385891987619962, articleId=1311999380052336675, language=CN, label=表5, caption=
区域−流域单元各地层线分形特征
, figureFileSmall=null, figureFileBig=null, tableContent=
| 级次 | 分形特征 | 地层代号 |
| Є2qn | Є1t | Є1sl | Є1s | Z2dn |
| 流域单元 | 分维值 | 0.8170 | 0.8589 | 0.9008 | 0.8607 | 0.8954 |
| 区域单元 | 0.9399 | 0.9589 | 1.0475 | 1.0137 | 1.0242 |
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