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Evaluation of the feasibility of recovering the magma chamber's parameters by 3D Bayesian statistical inversion of synthetic MT data

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Języki publikacji
EN
Abstrakty
EN
Feasibility of recovering the magma chamber's parameters by 3D Bayesian statistical inversion of magnetotelluric data is estimated for the simplified conductivity model of the Vesuvios volcano. The results indicate that in the lack of prior information and data, the most efficient approach may consist in successive estimation of the geometry and the depth of the anomaly followed by estimation of the electric conductivity distribution in it. The horizontal boundaries of the target could be outlined by the high gradients of the impedance determinant phase pseudosections determined by the upward analytical continuation of the anomalous electromagnetic fields from the relief surface to the artificial reference plane located above the summit of the volcano. The vertical boundaries and the target extension as well as the electric conductivity could be estimated successively by means of 3D Bayesian statistical inversion of the collected magnetotelluric data carried out in the domain delimited by the estimated horizontal boundaries.
Słowa kluczowe
Czasopismo
Rocznik
Strony
942--958
Opis fizyczny
Bibliogr. 27 poz.
Twórcy
autor
  • Geoelectromagnetic Research Centre IPE RAS, Troitsk, Moscow Region, Russia, v.spichak@mail.ru
Bibliografia
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  • Manzella, A., G. Volpi, A. Zaja, and M. Meju (2004), Combined TEM-MT investigation of shallow-depth resistivity structure of Mt Somma-Vesuvius, J. Volcanol. Geoth. Res. 131, 1-2, 19-32, DOI: 10.1016/S0377-0273(03)00313-5.
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  • Mogi, T., and K. Nakama (1990), Three-dimensional geoelectrical structure of geothermal system in Kuju volcano and its interpretation, Geoth. Res. Council Trans. 14, part II, 1513-1515.
  • Moroz, Y.F., V.I. Kobzova, I.P. Moroz, and A.F. Senchina (1988), Analogue modeling of MT-fields of volcano, Vulkanol. Seismol. 3, 98-104 (in Russian).
  • Newman, G.A., P.E. Wannamaker, and G.W. Hohmann (1985), On the detectability of crustal magma chambers using the magnetotelluric method, Geophysics 50, 7, 1136-1143, DOI: 10.1190/1.1441987.
  • Park, S.K., and C. Torres-Verdin (1988), A systematic approach to the interpretation of magnetotelluric data in volcanic environments with applications to the quest for magma in Long Valley, California, J. Geophys. Res. 93, B11, 13265-13283, DOI: 10.1029/JB093iB11p13265.
  • Press, S.J. (1989), Bayesian Statistics: Principles, Models and Applications, John Wiley and Sons, New York.
  • Siripunvaraporn, W. (2012), Three-dimensional magnetotelluric inversion: An introductory guide for developers and users, Surv. Geophys. 33, 1, 5-27, DOI: 10.1007/s10712-011-9122-6.
  • Spichak, V.V. (1999), Imaging of volcanic interior using MT data. In: M. Oristaglio and B. Spies (eds.), 3D Electromagnetics, Geophys. Devel. Ser. 7, Soc. Explor. Geophys. Publ., Tulsa, 418-425.
  • Spichak, V.V. (2001), Three-dimensional interpretation of MT data in volcanic environments (computer simulation), Ann. Geofis. 44, 2, 273-286.
  • Spichak, V.V. (2002), Advanced three-dimensional interpretation technologies applied to the MT data in the Minamikayabe thermal area (Hokkaido, Japan), In: Proc. EAGE 64th Conference and Exhibition, 27-30 May 2002, Florence, Italy, 243-246.
  • Spichak, V.V. (2007), Modeling of magnetotelluric fields in 3-D media. In: V.V. Spichak (ed.), Electromagnetic Sounding of the Earth’s Interior, Elsevier, Amsterdam, 313-350, DOI: 10.1016/S0076-6895(06)40012-3.
  • Spichak, V.V., and I. Popova (2000), Artificial neural network inversion of magnetotelluric data in terms of three-dimensional earth macroparameters, Geophys. J. Int. 142, 1, 15-26, DOI: 10.1046/j.1365-246x.2000.00065.x.
  • Spichak, V.V., and M.S. Zhdanov (2007), 3-D EM forward modeling using balance technique. In: V.V. Spichak (ed.), Electromagnetic Sounding of the Earth’s Interior, Elsevier, Amsterdam, 105-142, DOI: 10.1016/S0076-6895(06)40005-6.
  • Spichak, V.V., M. Menvielle, and M. Roussignol (1999a), Three-dimensional inversion of MT fields using Bayesian statistics. In: M. Oristaglio and B. Spies (eds.), 3D Electromagnetics, Geophys. Devel. Ser. 7, Soc. Explor. Geophys. Publ., Tulsa, 406-417.
  • Spichak, V.V., M. Menvielle, and M. Roussignol (1999b), Estimation of the effects of quality and volume of a priori information and data on 3-D inversion of magnetotelluric fields, Izv. – Phys. Solid Earth 35, 4, 260-270.
  • Spichak, V.V., Y. Yamaya, and T. Mogi (2004), ANN modeling of 3D conductivity structure of the Komagatake volcano (Hokkaido, Japan) by MT data. In: Proc. IV Int. Symp. MEEMSV 2004, La Londe Les Maures, France, 121-122.
  • Spichak, V.V., V.P. Borisova, E.B. Fainberg, A.A. Khalezov, and A.G. Goidina (2007), Electromagnetic 3D tomography of the Elbrus volcanic center according to magnetotelluric and satellite data, J. Volcanol. Seismol. 1, 1, 53-66, DOI: 10.1134/S0742046307010046.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL4-0017-0026
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