收缩条件下的移动页岩建模:对页岩构造新模拟的批判性分析以及与含盐系统的比较

Tim P. Dooley, Juan I. Soto, Jacqueline E. Reber, Michael R. Hudec, Frank J. Peel, Gillian M. Apps
{"title":"收缩条件下的移动页岩建模:对页岩构造新模拟的批判性分析以及与含盐系统的比较","authors":"Tim P. Dooley, Juan I. Soto, Jacqueline E. Reber, Michael R. Hudec, Frank J. Peel, Gillian M. Apps","doi":"10.1190/int-2024-0025.1","DOIUrl":null,"url":null,"abstract":"Weak substrates, such as salt and mobile shales, exert a strong control on deformation styles in all structural settings, especially those undergoing contraction. Despite both materials being very weak, they are mechanically very different. Salt is weak and will flow in a ductile fashion under most geologic conditions, whereas shales only become mobile after reaching critical state. Many sandbox-style physical or analog modeling studies have typically utilized a salt analog, viscous silicone polymer, as a proxy for mobile shales. However, to more accurately model mobile shale behavior the model material needs to exhibit a yield strength. One such material is Carbopol which is made up of micro-gel grains that are elasto-plastic, separated by a viscous interstitial ?uid. The abundance of the grains depends on the concentration of the mixture. Our results show that Carbopol does behave much differently than the traditional salt analog during contraction. PDMS typically undergoes bulk deformation and inflation under contraction, whereas Carbopol forms discrete, intense shear zones, and contains zones of little to no strain where its yield strength has not been exceeded. Below the shale analog, brittle layers typically form imbricate thrust stacks, jacking up the overburden, with shear zones propagating out from thrust tips along and through the shale proxy. Strain analyses reveal complex switching of activity within the Carbopol and overlying sediments. Models reveal that even a very thin layer of Carbopol can act as a highly-efficient detachment, and form more geologically realistic shortening structures, especially where these detachments are vertically stacked and horizontally offset. We believe that Carbopol is a powerful mobile-shale analog and opens new modeling directions because, as far as we are aware, this material has never been incorporated into a traditional sandbox model. Future work will seek to incorporate this material into more complex and three-dimensional sandbox-style models.","PeriodicalId":502519,"journal":{"name":"Interpretation","volume":"29 3","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-05-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"MODELING MOBILE SHALES UNDER CONTRACTION: CRITICAL ANALYSES OF NEW ANALOG SIMULATIONS OF SHALE TECTONICS AND COMPARISON WITH SALT-BEARING SYSTEMS\",\"authors\":\"Tim P. Dooley, Juan I. Soto, Jacqueline E. Reber, Michael R. Hudec, Frank J. Peel, Gillian M. Apps\",\"doi\":\"10.1190/int-2024-0025.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Weak substrates, such as salt and mobile shales, exert a strong control on deformation styles in all structural settings, especially those undergoing contraction. Despite both materials being very weak, they are mechanically very different. Salt is weak and will flow in a ductile fashion under most geologic conditions, whereas shales only become mobile after reaching critical state. Many sandbox-style physical or analog modeling studies have typically utilized a salt analog, viscous silicone polymer, as a proxy for mobile shales. However, to more accurately model mobile shale behavior the model material needs to exhibit a yield strength. One such material is Carbopol which is made up of micro-gel grains that are elasto-plastic, separated by a viscous interstitial ?uid. The abundance of the grains depends on the concentration of the mixture. Our results show that Carbopol does behave much differently than the traditional salt analog during contraction. PDMS typically undergoes bulk deformation and inflation under contraction, whereas Carbopol forms discrete, intense shear zones, and contains zones of little to no strain where its yield strength has not been exceeded. Below the shale analog, brittle layers typically form imbricate thrust stacks, jacking up the overburden, with shear zones propagating out from thrust tips along and through the shale proxy. Strain analyses reveal complex switching of activity within the Carbopol and overlying sediments. Models reveal that even a very thin layer of Carbopol can act as a highly-efficient detachment, and form more geologically realistic shortening structures, especially where these detachments are vertically stacked and horizontally offset. We believe that Carbopol is a powerful mobile-shale analog and opens new modeling directions because, as far as we are aware, this material has never been incorporated into a traditional sandbox model. Future work will seek to incorporate this material into more complex and three-dimensional sandbox-style models.\",\"PeriodicalId\":502519,\"journal\":{\"name\":\"Interpretation\",\"volume\":\"29 3\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-05-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Interpretation\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1190/int-2024-0025.1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Interpretation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1190/int-2024-0025.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

盐和流动页岩等弱基质对所有构造环境中的变形方式都有很强的控制作用,尤其是那些正在发生收缩的构造环境。尽管这两种材料都非常软弱,但它们在力学上却有很大不同。盐很薄弱,在大多数地质条件下都会以韧性方式流动,而页岩只有在达到临界状态后才会具有流动性。许多沙箱式物理或模拟建模研究通常使用盐的类似物--粘性硅聚合物--来替代流动页岩。然而,为了更准确地模拟流动页岩的行为,模型材料需要表现出屈服强度。Carbopol 就是这样一种材料,它由具有弹性的微凝胶颗粒组成,并由粘性间隙液隔开。颗粒的丰度取决于混合物的浓度。我们的研究结果表明,Carbopol在收缩过程中的表现与传统的盐类似物大不相同。在收缩过程中,PDMS通常会发生整体变形和膨胀,而Carbopol则会形成离散、强烈的剪切区,并在未超过屈服强度的地方形成几乎没有应变的区域。在页岩模拟物下方,脆性层通常形成错综复杂的推力层,将覆盖层顶起,剪切带从推力顶端沿页岩代理层传播出去并穿过页岩代理层。应变分析揭示了 Carbopol 和上覆沉积物内部复杂的活动转换。模型显示,即使是很薄的Carbopol层也能起到高效剥离的作用,并形成更符合地质实际的缩短结构,尤其是在这些剥离垂直叠加、水平偏移的情况下。我们认为,Carbopol是一种强大的移动页岩模拟材料,开辟了新的建模方向,因为据我们所知,这种材料从未被纳入传统的沙盘模型中。未来的工作将寻求将这种材料纳入更复杂的三维沙箱式模型中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
MODELING MOBILE SHALES UNDER CONTRACTION: CRITICAL ANALYSES OF NEW ANALOG SIMULATIONS OF SHALE TECTONICS AND COMPARISON WITH SALT-BEARING SYSTEMS
Weak substrates, such as salt and mobile shales, exert a strong control on deformation styles in all structural settings, especially those undergoing contraction. Despite both materials being very weak, they are mechanically very different. Salt is weak and will flow in a ductile fashion under most geologic conditions, whereas shales only become mobile after reaching critical state. Many sandbox-style physical or analog modeling studies have typically utilized a salt analog, viscous silicone polymer, as a proxy for mobile shales. However, to more accurately model mobile shale behavior the model material needs to exhibit a yield strength. One such material is Carbopol which is made up of micro-gel grains that are elasto-plastic, separated by a viscous interstitial ?uid. The abundance of the grains depends on the concentration of the mixture. Our results show that Carbopol does behave much differently than the traditional salt analog during contraction. PDMS typically undergoes bulk deformation and inflation under contraction, whereas Carbopol forms discrete, intense shear zones, and contains zones of little to no strain where its yield strength has not been exceeded. Below the shale analog, brittle layers typically form imbricate thrust stacks, jacking up the overburden, with shear zones propagating out from thrust tips along and through the shale proxy. Strain analyses reveal complex switching of activity within the Carbopol and overlying sediments. Models reveal that even a very thin layer of Carbopol can act as a highly-efficient detachment, and form more geologically realistic shortening structures, especially where these detachments are vertically stacked and horizontally offset. We believe that Carbopol is a powerful mobile-shale analog and opens new modeling directions because, as far as we are aware, this material has never been incorporated into a traditional sandbox model. Future work will seek to incorporate this material into more complex and three-dimensional sandbox-style models.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
×
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