Depth–Strength In-Situ Stress Model for Granite in Southeastern Tibetan Plateau and Its Implications for Stress Estimation in the Upper Crust

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Junshan Xu, Xiwei Xu
{"title":"Depth–Strength In-Situ Stress Model for Granite in Southeastern Tibetan Plateau and Its Implications for Stress Estimation in the Upper Crust","authors":"Junshan Xu,&nbsp;Xiwei Xu","doi":"10.1007/s00024-024-03591-0","DOIUrl":null,"url":null,"abstract":"<div><p>Extracting the effective information of a tectonic stress field from in-situ stress data is significantly important for engineering projects and solid Earth sciences but extremely difficult to perform because of the scattered distribution of stress data and the complexity of rock mechanical properties. A depth–strength in-situ stress model is proposed in this study by deriving the local maximum horizontal strain (<i>ε</i><sub><i>H</i></sub>) via an analysis of the depth trend of the maximum horizontal principal stress (<i>S</i><sub><i>H</i></sub>) for granite in the southeastern Tibetan Plateau (SETP). In this model, the depth trend of <i>S</i><sub><i>H</i></sub> is divided into three segments in accordance with the values of <i>S</i><sub><i>H</i></sub> and the variations in rock mechanical properties. The first segment (0–15 MPa) shows the complexity of <i>S</i><sub><i>H</i></sub> affected by multiple factors of local settings on the near-surface. The second segment (15–45 MPa) exhibits the slope of <i>S</i><sub><i>H</i></sub> against depth mainly caused by elastic variations against the decrease in porosity (or fracture closure) and increase in pressure. The third segment (&gt; 45 MPa) explains the stable depth trend of <i>S</i><sub><i>H</i></sub> in relation to the increase in pressure only. The <i>ε</i><sub><i>H</i></sub> can be extracted using the second segment, and it is in the range of 4 × 10<sup>−4</sup>–6 × 10<sup>−4</sup> in the granite area of the SETP. The depth trend of stress in the shallow layer of the crust calculated based on the extracted <i>ε</i><sub><i>H</i></sub> is consistent with that from in-situ stress measurements. Moreover, the stress distribution along the Xianshuihe fault calculated based on the extracted <i>ε</i><sub><i>H</i></sub> suggests that the values of differential stress range within 200–250 MPa at a depth range of 10–16 km, a result that agrees well with local focal depths. The proposed model connects the in-situ stress in the shallow layers with the tectonic stress environment in the deep crust.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 10","pages":"3103 - 3120"},"PeriodicalIF":1.9000,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"pure and applied geophysics","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00024-024-03591-0","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Extracting the effective information of a tectonic stress field from in-situ stress data is significantly important for engineering projects and solid Earth sciences but extremely difficult to perform because of the scattered distribution of stress data and the complexity of rock mechanical properties. A depth–strength in-situ stress model is proposed in this study by deriving the local maximum horizontal strain (εH) via an analysis of the depth trend of the maximum horizontal principal stress (SH) for granite in the southeastern Tibetan Plateau (SETP). In this model, the depth trend of SH is divided into three segments in accordance with the values of SH and the variations in rock mechanical properties. The first segment (0–15 MPa) shows the complexity of SH affected by multiple factors of local settings on the near-surface. The second segment (15–45 MPa) exhibits the slope of SH against depth mainly caused by elastic variations against the decrease in porosity (or fracture closure) and increase in pressure. The third segment (> 45 MPa) explains the stable depth trend of SH in relation to the increase in pressure only. The εH can be extracted using the second segment, and it is in the range of 4 × 10−4–6 × 10−4 in the granite area of the SETP. The depth trend of stress in the shallow layer of the crust calculated based on the extracted εH is consistent with that from in-situ stress measurements. Moreover, the stress distribution along the Xianshuihe fault calculated based on the extracted εH suggests that the values of differential stress range within 200–250 MPa at a depth range of 10–16 km, a result that agrees well with local focal depths. The proposed model connects the in-situ stress in the shallow layers with the tectonic stress environment in the deep crust.

求助全文
约1分钟内获得全文 求助全文
来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信