Lithospheric plane strain deformation due to tensile faulting.

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Title: Lithospheric plane strain deformation due to tensile faulting.
Authors: Soni, Nirmal1 (AUTHOR), Rani, Sunita1 (AUTHOR) srani@rediffmail.com, Bala, Neeru2 (AUTHOR)
Source: Earthquake Engineering & Engineering Vibration. Apr2025, Vol. 24 Issue 2, p301-309. 9p.
Subjects: Strains & stresses (Mechanics), Exponential sums, Least squares, Barite, Olivine
Abstract: A solution for the lithospheric deformation of a uniform, elastically isotropic layer (EIL) of uniform thickness welded with a uniform, elastically orthotropic half-space (EOHS) due to a vertical tensile line fault (VTLF) with an opening in the horizontal direction located in the isotropic layer is derived in the integral form by employing Airy's stress function approach for the plane strain case. The linear combination of exponential terms appearing in the denominator of the integral expressions of the deformation field of the EIL is expressed as a finite sum of exponential terms (FSET) by applying the method of least squares to analytically compute the deformation field. The displacement field is discussed in detail and computed numerically by considering the EOHS as olivine or barytes material or considering half-space to be isotropic. [ABSTRACT FROM AUTHOR]
Copyright of Earthquake Engineering & Engineering Vibration is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: <searchLink fieldCode="JN" term="%22Earthquake+Engineering+%26+Engineering+Vibration%22">Earthquake Engineering & Engineering Vibration</searchLink>. Apr2025, Vol. 24 Issue 2, p301-309. 9p.
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  Data: A solution for the lithospheric deformation of a uniform, elastically isotropic layer (EIL) of uniform thickness welded with a uniform, elastically orthotropic half-space (EOHS) due to a vertical tensile line fault (VTLF) with an opening in the horizontal direction located in the isotropic layer is derived in the integral form by employing Airy's stress function approach for the plane strain case. The linear combination of exponential terms appearing in the denominator of the integral expressions of the deformation field of the EIL is expressed as a finite sum of exponential terms (FSET) by applying the method of least squares to analytically compute the deformation field. The displacement field is discussed in detail and computed numerically by considering the EOHS as olivine or barytes material or considering half-space to be isotropic. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Earthquake Engineering & Engineering Vibration is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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        Value: 10.1007/s11803-025-2312-x
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        Text: English
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      – SubjectFull: Exponential sums
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      – TitleFull: Lithospheric plane strain deformation due to tensile faulting.
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              Text: Apr2025
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              Y: 2025
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