Three-dimensional Magnetotelluric Modeling of data from Northeast of Gorgan Plain

نوع مقاله : مقاله پژوهشی‌

نویسندگان

1 موسسسه ژئوفیزیک دانشگاه تهران، تهران، ایران

2 موسسه ژئوفیزیک دانشگاه تهران، تهران، ایران

چکیده

Magnetotelluric measurements have been conducted in the period range of 0.005-128 s along five parallel east-west directed profiles including 85 sites totally in the north-eastern part of Gorgan Plain, Golestan Province, North of Iran; with the aim of exploring iodine. Distortion and dimensionality analysis of data imply the existence of a north-south elongated two-dimensional model with some localized three-dimensional effects, particularly at long periods, that has been mildly affected by non-inductive distortions. Exclusion of a very few data points with large values of distortion angles and rotation based on the selected azimuth of strike was followed by two-dimensional inversion of joint TE- and TM-mode apparent resistivity and phase data. After some resolution tests to ensure the reliability of the detected features, three-dimensional inversion of real and imaginary parts of full impedance tensor data was accomplished. Despite the reduced resolution of magnetotelluric data in a conductive environment, the elimination of part of the data due to hardware constraints and the lack of an ideal data acquisition pattern, the models showed some definite results. The resulted electrical resistivity models from both two- and three-dimensional inversion resolved highly conductive bodies as our exploration targets, which are expected to be saline aquifers containing iodine within the generally conductive sediments.

کلیدواژه‌ها

موضوعات


عنوان مقاله [English]

Three-dimensional Magnetotelluric Modeling of data from Northeast of Gorgan Plain

نویسندگان [English]

  • Omid Bagherpur 1
  • Banafsheh Habibian Dehkordy 2
  • Behrooz Oskooi 2
1 Department of Geophysics, Institute of Geophysics, University of Tehran, Tehran, Iran
2 Department of Geophysics, Institute of Geophysics, University of Tehran, Tehran, Iran
چکیده [English]

Magnetotelluric measurements have been conducted in the period range of 0.005-128 s along five parallel east-west directed profiles including 85 sites totally in the north-eastern part of Gorgan Plain, Golestan Province, North of Iran; with the aim of exploring iodine. Distortion and dimensionality analysis of data imply the existence of a north-south elongated two-dimensional model with some localized three-dimensional effects, particularly at long periods, that has been mildly affected by non-inductive distortions. Exclusion of a very few data points with large values of distortion angles and rotation based on the selected azimuth of strike was followed by two-dimensional inversion of joint TE- and TM-mode apparent resistivity and phase data. After some resolution tests to ensure the reliability of the detected features, three-dimensional inversion of real and imaginary parts of full impedance tensor data was accomplished. Despite the reduced resolution of magnetotelluric data in a conductive environment, the elimination of part of the data due to hardware constraints and the lack of an ideal data acquisition pattern, the models showed some definite results. The resulted electrical resistivity models from both two- and three-dimensional inversion resolved highly conductive bodies as our exploration targets, which are expected to be saline aquifers containing iodine within the generally conductive sediments.

کلیدواژه‌ها [English]

  • magnetotellurics
  • two- and three-dimensional inversion
  • iodine exploration
  • electrical conductivity
Ailes, C. E., and Rodriguez, B. D., 2015, Magnetotelluric data collected to characterize aquifers in the San Luis Basin, New Mexico: U. S. Geological Survey Open-File Report 2014–1248, 9 p., http://dx.doi.org/10.3133/ofr20141248.
Asaue, H., Kubo, T., Yoshinaga, T., and Koike, K., 2012, Application of magnetotelluric (MT) resistivity to imaging of regional three-dimensional geologic structures and groundwater systems: Natural Resources Research, 21(3), 383-393.
Caldwell, T. G., Bibby, H. M., and Brown, C., 2004, The magnetotelluric phase tensor: Geophysical Journal International, 158, 457-469.
Falgàs, E., Ledo, J., Teixidó, T., Gabàs, A., Ribera, F., Arango, C., Queralt, P., Plata, J. L., Rubio, F., Peña, J. A., Martí A., and Marcuello, A., 2005, Geophysical characterization of a Mediterranean costal aquifer, Baixa Tordera fluvial deltaic aquifer unit: Groundwater Saline Intrusion, 15, 395-404.
Groom, R. W., and Bailey, R. C., 1989, Decomposition of magnetotelluric impedance tensor in the presence of local three-dimensional galvanic distortions: Journal of Geophysical Research, 94, 1913-1925.
Hollingsworth, J., Jackson, J., Walker, R., Gheitanchi, M. R., and Bolourchi, M. J., 2006, Strike-slip faulting, rotation, and along-strike elongation in the Kopeh-Dagh mountains, NE Iran: Geophysical Journal International, 166, 1161-1177.
Juanatey, M. G., Hübert, J., Tryggvason, A., and Pedersen, L. B., 2013, Imaging the Kristineberg mining area with two perpendicular magnetotelluric profiles in the Skellefte Ore District, northern Sweden: Geophysical Prosoecting, 61, 200-219.
Marti, A., Queralt, P., and Ledo, J., 2009, WALDIM, A code for the dimensionality analysis of magnetotelluric data using the rotational invariants of the magnetotelluric tensor: Computers and Geosciences, 25, 2295–2303.
Mejiʹas, M., Garcia-Orellana, J., Plata, J. L., Marina, M., Garcia-Solsona, E., Ballesteros, B., Masque, P., Lopez, J., and Fernandez-Arrojo, C., 2008, Methodology of hydrogeological characterization of deep carbonate aquifers as potential reservoirs of groundwater: Case of study, the Jurassic aquifer of El Maestrazgo (Castellón, Spain): Environmental Geology, 54(3), 521–536.
Meliʹi, J. L., Njandjock, P. N., and Gouet, D. H., 2011, Magnetotelluric method for groundwater exploration in crystalline basement complex, Cameron: Journal of Environmental Hydrology, 19, x–y.
Oskooi, B., and Mansoori, I., 2015, Iodine-bearing saline aquifer prospecting using magnetotelluric method in Golestan plain, NE Iran: Arabian Journal of Geoscience, 8, 5959–5969.
Pedersen, L. B., Bastani, M., and Dynesius, L., 2005, Groundwater exploration using combined controlled-source and radiomagnetotelluric techniques: Geophysics, 70, G8-G15.
Siripunvaraporn, W., and Egbert, G., 2000, An efficient data-subspace inversion method for 2-D magnetotelluric data: Geophysics, 65 (3), 791-803.
Siripunvaraporn, W., Egbert, G., Lenbury, Y., and Uyeshima, M., 2005, Three-dimensional magnetotelluric inversion: data-space method: Physics of the Earth and Planetary Interiors, 150, 3–14.
Siripunvaraporn, W., Egbert, G., and Uyeshima, M., 2005, Interpretation of two-dimensional magnetotelluric profile data with three-dimensional inversion, synthetic examples: Geophysical Journal International, 160, 804–814.
Smirnov, M. Y., 2003, Magnetotelluric data processing with a robust statistical procedure having a high breakdown point: Geophysical Journal International, 152, 1–7.
Steuer, A., Helwig, S. L. and Tezkan, B., 2008, Aquifer characterization in the Quarzazate Basin (Morocco),: A contribution by TEM and RMT data: Near Surface Geophysics, x, 5–14.
Weaver, J. T., Agarwal, A. K., and Lilley, F. E. M., 2000, Characterization of the magnetotelluric tensor in terms of its invariants: Geophysical Journal International, 141, 321–336.