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- Changyou Zhang
- ∗Formerly Univ. of Leeds, School of Earth Sciences, Leeds LS2 9JT, UK; presently 117-401 Westview St., Coquitlam, British Columbia V3K 3W3, Canada.
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- Martin F. Mushayandebvu
- ‡Univ. of Leeds, School of Earth Sciences, Leeds LS2 9JT, UK. E-mail: mushaya@earth.leeds.ac.uk.
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- Alan B. Reid
- ∗∗Formerly GETECH, c/o Univ. of Leeds, School of Earth Sciences, Leeds; presently Reid Geophysics, 49 Carr Bridge Dr., Leeds LS16 7LB, UK. E-mail: alan@reidgeophys.freeserve.co.uk.
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- J. Derek Fairhead
- §GETECH, Univ. of Leeds, c/o School of Earth Sciences, Leeds LS2 9JT, UK. E-mail: jdf@getech.leeds.ac.uk.
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- Mark E. Odegard
- ††Formerly Unocal Corp. E&P Technology, USA, Sugar Land, Texas; presently GETECH Inc., 12946 Dairy Ashford Rd., Suite 250, Sugar Land, Texas 77478. E-mail: meo@getech.com.
書誌事項
- 公開日
- 1999-10-20
- DOI
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- 10.1190/1.1444745
- 公開者
- Society of Exploration Geophysicists
この論文をさがす
説明
<jats:title>Abstract</jats:title> <jats:p>Tensor Euler deconvolution has been developed to help interpret gravity tensor gradient data in terms of 3-D subsurface geological structure. Two forms of Euler deconvolution have been used in this study: conventional Euler deconvolution using three gradients of the vertical component of the gravity vector and tensor Euler deconvolution using all tensor gradients.</jats:p> <jats:p>These methods have been tested on point, prism, and cylindrical mass models using line and gridded data forms. The methods were then applied to measured gravity tensor gradient data for the Eugene Island area of the Gulf of Mexico using gridded and ungridded data forms. The results from the model and measured data show significantly improved performance of the tensor Euler deconvolution method, which exploits all measured tensor gradients and hence provides additional constraints on the Euler solutions.</jats:p>
収録刊行物
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- Geophysics
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Geophysics 65 (2), 512-520, 1999-10-20
Society of Exploration Geophysicists