Relevant bibliographies by topics / Conductivity anomaly

Academic literature on the topic 'Conductivity anomaly'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Conductivity anomaly"

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Parkinson, W. D., and R. Hermanto. "The Tamar conductivity anomaly." Exploration Geophysics 17, no. 1 (March 1986): 34–35. http://dx.doi.org/10.1071/eg986034.

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Parkinson, W. D., R. Hermanto, J. Sayers, N. L. Bindoff, H. W. Dosso, and W. Nienaber. "The Tamar conductivity anomaly." Physics of the Earth and Planetary Interiors 52, no. 1-2 (October 1988): 8–22. http://dx.doi.org/10.1016/0031-9201(88)90053-2.

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Schäfer, A., L. Houpt, H. Brasse, and N. Hoffmann. "The North German Conductivity Anomaly revisited." Geophysical Journal International 187, no. 1 (August 24, 2011): 85–98. http://dx.doi.org/10.1111/j.1365-246x.2011.05145.x.

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AMMARI, HABIB, FAOUZI TRIKI, and CHUN-HSIANG TSOU. "Numerical determination of anomalies in multifrequency electrical impedance tomography." European Journal of Applied Mathematics 30, no. 3 (May 17, 2018): 481–504. http://dx.doi.org/10.1017/s0956792518000244.

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The multifrequency electrical impedance tomography consists in retrieving the conductivity distribution of a sample by injecting a finite number of currents with multiple frequencies. In this paper, we consider the case where the conductivity distribution is piecewise constant, takes a constant value outside a single smooth anomaly, and a frequency dependent function inside the anomaly itself. Using an original spectral decomposition of the solution of the forward conductivity problem in terms of Poincaré variational eigenelements, we retrieve the Cauchy data corresponding to the extreme case of a perfect conductor, and the conductivity profile. We then reconstruct the anomaly from the Cauchy data. The numerical experiments are conducted using gradient descent optimization algorithms.
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Milligan, P. R., A. White, and F. H. Chamalaun. "Extension of the Eyre Peninsula Conductivity Anomaly." Exploration Geophysics 20, no. 2 (1989): 187. http://dx.doi.org/10.1071/eg989187.

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Twenty-two digitally recording fluxgate magnetometers measuring short-period natural time variations of the geomagnetic field were deployed during 1988 at 54 sites to define the northward extension of the Eyre Peninsula Conductivity Anomaly (EPCA). The southern portion of this zone of high electrical conductivity was initially mapped during the early 1980s; it trends inland just to the east of north from the southern extremity of the peninsula, at nearly 90� to the continental shelf edge.The 1988 data show that the axis of the anomaly in the north initially swings to the east, and then turns NNW, following the major structural trends in the Precambrian basement of the Gawler Block. Short-period geomagnetic variations observed in stacked magnetograms display a significant amplitude and phase change in the vertical (Z) and total field (F) components across the anomaly axis, while the horizontal variation fields (D and H) are enhanced along the axis. These features are consistent with a concentration of current in the crust.Transfer-functions relating the anomalous vertical to normal horizontal geomagnetic variation fields are expressed in the form of vectors and hypothetical event contours, and these clearly delineate the surface position of the anomaly axis.The EPCA is coincident with a broad band of seismic activity, and a continuous conductive zone such as this must be formed along a significant structure within the Precambrian crust. The zone probably delineates the boundary between the essentially non-conductive Archean crystalline basement to the west and the multiply deformed Proterozoic metasediments of the Hutchison Group to the east. Its presence is important in understanding the tectonic development of this potentially economic zone.Zones such as the EPCA can also introduce errors of several nT into aeromagnetic surveys; data from closely-spaced magnetometer arrays may be used to accurately predict and eliminate such errors.
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Cann, David P., Ross Martin, Christi Taylor, and Naratip Vittayakorn. "Conductivity anomaly in CuInGaO4 and CuIn2Ga2O7 ceramics." Materials Letters 58, no. 16 (June 2004): 2147–51. http://dx.doi.org/10.1016/j.matlet.2004.01.013.

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Kumar, Pradeep, and H. Eugene Stanley. "Thermal Conductivity Minimum: A New Water Anomaly." Journal of Physical Chemistry B 115, no. 48 (December 8, 2011): 14269–73. http://dx.doi.org/10.1021/jp2051867.

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Sauer, H. M. "On a conductivity anomaly in nanoscaled metals." Nanostructured Materials 6, no. 5-8 (January 1995): 759–62. http://dx.doi.org/10.1016/0965-9773(95)00169-7.

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Mao, Zhiqiang, Chieh-Hung Chen, Suqin Zhang, Aisa Yisimayili, Huaizhong Yu, Chen Yu, and Jann-Yenq Liu. "Locating Seismo-Conductivity Anomaly before the 2017 MW 6.5 Jiuzhaigou Earthquake in China Using Far Magnetic Stations." Remote Sensing 12, no. 11 (June 1, 2020): 1777. http://dx.doi.org/10.3390/rs12111777.

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Changes in the underlying conductivity around hypocenters are generally considered one of the promising mechanisms of seismo-electromagnetic anomaly generation. Parkinson vectors are indicators of high-conductivity materials and were utilized to remotely monitor conductivity changes during the MW 6.5 Jiuzhaigou earthquake (103.82°E, 33.20°N) on 8 August 2017. Three-component geomagnetic data recorded in 2017 at nine magnetic stations with epicenter distances of 63–770 km were utilized to compute the azimuths of the Parkinson vectors based on the magnetic transfer function. The monitoring and background distributions at each station were constructed by using the azimuths within a 15-day moving window and over the entire study period, respectively. The background distribution was subtracted from the monitoring distribution to mitigate the effects of underlying inhomogeneous electric conductivity structures. The differences obtained at nine stations were superimposed and the intersection of a seismo-conductivity anomaly was located about 70 km away from the epicenter about 17 days before the earthquake. The anomaly disappeared about 7 days before and remained insignificant after the earthquake. Analytical results suggested that the underlying conductivity close to the hypocenter changed before the Jiuzhaigou earthquake. These changes can be detected simultaneously by using multiple magnetometers located far from the epicenter. The disappearance of the seismo-conductivity anomaly after the earthquake sheds light on a promising candidate of the pre-earthquake anomalous phenomena.
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Zhang, Xuan, Zhao-Xi Wang, Haomiao Xie, Ming-Xing Li, Toby J. Woods, and Kim R. Dunbar. "A cobalt(ii) spin-crossover compound with partially charged TCNQ radicals and an anomalous conducting behavior." Chemical Science 7, no. 2 (2016): 1569–74. http://dx.doi.org/10.1039/c5sc03547c.

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Dissertations / Theses on the topic "Conductivity anomaly"

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Ningelgen, Oliver Peter. "GoC : Gulf of Carpentaria electrical conductivity anomaly experiment /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbn7149g.pdf.

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陳伯舫 and Pak-fong Chan. "Numerical investigations of the terrestrial conductivity anomaly undervarious geophysical conditions." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1988. http://hub.hku.hk/bib/B31231494.

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Chan, Pak-fong. "Numerical investigations of the terrestrial conductivity anomaly under various geophysical conditions /." [Hong Kong : University of Hong Kong], 1988. http://sunzi.lib.hku.hk/hkuto/record.jsp?B12428577.

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Branch, Thomas Cameron. "Electrical conductivity experiments on carbon-rich Karoo shales and forward modelling of aeromagnetic data across the Beattie Anomaly." Thesis, Nelson Mandela Metropolitan University, 2014. http://hdl.handle.net/10948/d1014544.

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The Beattie Magnetic Anomaly is the world’s longest terrestrial magnetic anomaly with a strike length of over 1000 km and a wavelength in excess of 100 km. Collinear with this is a large belt of elevated crustal conductivities called the Southern Cape Conductive Belt. Historical crustal interpretations proposed a common source of serpentinized ophiolite as an explanation for both the anomalous crustal magnetic susceptibility and electrical conductivities. Spreading between the Western and Eastern Cape of South Africa the mid- to lower crust that hosts these anomalies is obscured by the overlying Cape and Karoo Supergroups. Between 2003 and 2006, three high resolution geophysical experiments were completed across the surface maximum of the Beattie Magnetic Anomaly (BMA) and the Southern Cape Conductive Belt (SCCB). These included a magnetotelluric (MT) survey and near vertical reflection and wide angle refraction seismic profiles. Within the MT inversion model the SCCB appeared as a composite anomaly, which included a mid-crustal conductor which is spatially associated with the BMA and a laterally continuous upper crustal conductor which is located at depths equivalent to the lower Karoo Supergroup. Subsequently; the upper crustal conductor was identified in northern and eastern extensions of the magnetotelluric profile; a distance in excess of 400 km. Historical magnetometer and Schlumberger Sounding experiments have previously identified elevated conductivities in the Karoo sequences which were attributed to the Whitehill and Prince Albert formations. These carboniferous, transgressive sediments are known to be conductive from borehole conductivity surveys and direct measurements at surface. In order to constrain the conductive properties of these sediments, impedance spectroscopy (IS) experiments were completed on core samples collected from a historical borehole drilled near to the MT profile. Part One of this thesis presents the results of these experiments, which support the proposition that the Whitehill and Prince Albert Formations are responsible for the laterally continuous, sub-horizontal, upper crustal conductor visible in the MT inversion model. Vitrinite reflectance studies were performed on the same samples by the Montanuniversität, in Leoben, these results corroborate the proposition that elevated organic carbon, of meta-anthracite rank, is the primary conductive phase for the Whitehill and Prince Albert formations. Part two of this thesis completed forward modelling exercises using historical aeromagnetic data previously collected across the Beattie Magnetic Anomaly. Preliminary models were unable to fit the geometry of any single magnetic model with conductors present in the MT inversion model discounting the proposition that the SCCB and BMA arise from a single crustal unit. Two constrained models were arrived at through an iterative process that sought a best fit between the measured data and the NVR crustal interpretations. The first model, proposes a largely resistive unit which incorporates portions of elevated crustal conductivity; these conductors are spatially correlated to crustal portions also characterised by high seismic reflectivity. The size of this modelled body suggest the likely host of the BMA is an intermediate plutonic terrane, analogous with the Natal sector of the Namaqua Natal Mobile Belt as well as the Heimefrontfjella in Dronning Maud Land, Antarctica, with magnetite hosted within shear zones. This is in agreement with previous studies. The second model proposes a lower crustal sliver imaged in the NVR data at depths proximal to the Curie Isotherm for magnetite and hematite as the source of the BMA. At these depths geomagnetic properties such as burial magnetisation or thermo-viscous remanent magnetism (TVRM) can potentially be linked to regional scale tectonic processes and can theoretically elevate a body’s net magnetic susceptibility. TVRM has been proposed for long wavelength crustal anomalies elsewhere.
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Kämmlein, Marion [Verfasser], Harald [Akademischer Betreuer] Stollhofen, Harald [Gutachter] Stollhofen, and Wall Helga [Gutachter] de. "The Franconian Basin temperature anomaly, SE Germany: Methodologically aspects on the determination of rock thermal conductivity and modelling of potential heat sources / Marion Kämmlein ; Gutachter: Harald Stollhofen, Helga de Wall ; Betreuer: Harald Stollhofen." Erlangen : Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU), 2020. http://d-nb.info/1205975292/34.

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Loader, L. "The Eyre Peninsula conductivity anomaly, South Australia." Thesis, 2018. http://hdl.handle.net/2440/130629.

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A major electrically conducting structure has been spatially located in the southern Eyre Peninsula, South Australia. The structure extends from the continental margin inland along the eastern margin of the Eyre Peninsula, trending north-northeast for approximately 150 km. In order to provide a two-dimensional image of the crust orthogonal to the conductor’s strike, 39 broadband (1000 to 0.01 Hz) magnetotelluric sites were collected with approximately 2 km separation across the peninsula. A smoothed 2-D inversion model demonstrated that the conductor appears centred beneath a topographic high, structurally bound at the east by the transpressional Kalinjala Shear Zone and resistive Donington Suite granitoids, and the Sleaford Complex to the west. The main features from modelling are: (i) east of the Kalinjala Shear Zone, a region of high resistivity (> 1000 ohm/m) relates to the Donington Suite granitoids; (ii) the late Archaean Sleaford Complex (2480–2420 Ma) bordering the Donington Suite granitoids features a lower, wider resistivity range between 5 to < 600 ohm/m, and is near-vertical in the top 12 km; (iii) the lowest resistivity structure of < 0.1 ohm/m occurs at a depth of 5-10 km, and appears to terminate at a depth of ~15 km; (iv) the low resistivity structure correlates with banded iron formations and is credibly the result of biogenically deposited graphite in marine sediments, which migrated to become concentrated in fold hinges during the Kimban Orogeny; and (iv) the conductor is co-located with a ridge of high gravity (+ 200 to 500 mGals). The origin of this high gravity may be due to a mafic intrusive block of oceanic crust, compressed during the continental collision of the Kimban Orogeny. Utilising the constraints of the 2-D model, a regional 3-D forward model was developed which shows agreement with compiled legacy data sets.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2018
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Dello-Iacovo, M. "South Australian Heat Flow Anomaly: source and implications for geothermal energy." Thesis, 2014. http://hdl.handle.net/2440/109977.

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The South Australian Heat Flow Anomaly is a broad region (>400 km wide) in Proterozoic South Australia defined by drill holes with anomalously high heat flow estimates yielding a mean of 92 +/- 10 mW m−2, compared to a global Proterozoic mean of 49-54 mW m−2. This study will conclusively determine the primary source of this anomalous heat flow. Thermal conductivities of 145 drill core samples have been measured using an optical thermal conductivity scanner. These were utilised with thermal conductivity and temperature profiles provided by Petratherm and the Department of State Development to make five new heat flow estimates in the Curnamona and Mount Painter provinces using the product and thermal resistance methods. Measured surface heat flows fall between 84.352 and 128.051 mW m−2. Significant lateral variations in surface heat flow support previous work suggesting shallow crustal radiogenic heat generation, primarily in Mesoproterozoic high heat producing granites. Analysis of existing deep seismic data has revealed a significantly cooler and thicker lithosphere in the Proterozoic South Australia compared with regions dominated by mantle heat flow such as southeastern Australia. Geotherms have been computed for steady-state regimes to demonstrate that the surface heat flow evident in the South Australian Heat Flow Anomaly is consistent with elevated upper crustal source. Thick, thermally insulating sedimentary cover in the Curnamona and Mount Painter provinces and high temperatures at shallow depths are encouraging for geothermal energy exploration, and geothermal prospectivity for these provinces was examined. Lateral thermal conductivity variations of stratigraphies in the Curnamona Province have been assessed, revealing that more data must be collected to use thermal conductivity from neighbouring boreholes as a proxy for heat flow estimates.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2014
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Books on the topic "Conductivity anomaly"

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Sergeenkov, Sergei. 2D arrays of Josephson nanocontacts and nanogranular superconductors. Edited by A. V. Narlikar and Y. Y. Fu. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199533046.013.21.

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This article examines many novel effects related to the magnetic, electric, elastic and transport properties of Josephson nanocontacts and nanogranular superconductors using a realistic model of two-dimensional Josephson junction arrays. The arrays were created by a 2D network of twin-boundary dislocations with strain fields acting as an insulating barrier between hole-rich domains in underdoped crystals. The article first describes a model of nanoscopic Josephson junction arrays before discussing some interesting phenomena, including chemomagnetism and magnetoelectricity, electric analog of the ‘fishtail‘ anomaly and field-tuned weakening of the chemically induced Coulomb blockade, a giant enhancement of the non-linear thermal conductivity in 2D arrays, and thermal expansion of a singleJosephson contact.
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Book chapters on the topic "Conductivity anomaly"

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Rikitake, Tsuneji. "Conductivity Anomaly of the Upper Mantle." In The Earth's Crust and Upper Mantle, 463–69. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0463.

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Sternberg, Ben K., and C. S. Clay. "Flambeau Anomaly: A High-Conductivity Anomaly in the Southern Extension of the Canadian Shield." In Geophysical Monograph Series, 501–30. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm020p0501.

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Watanabe, T., and A. Matsuda. "One-Dimensional Conductivity and Resistivity Anomaly Observed in La8-xSrxCu8O20 Single Crystals." In Springer Proceedings in Physics, 267–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77154-5_53.

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Zhamaletdinov, A. A., I. I. Rokityansky, and E. Yu Sokolova. "Evolution of Ideas on the Nature and Structure of Ladoga Anomaly of Electrical Conductivity." In Springer Proceedings in Earth and Environmental Sciences, 197–206. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-97670-9_23.

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Koyama, Takao, Hisayoshi Shimizu, Hisashi Utada, Masahiro Ichiki, Eiji Ohtani, and Ryota Hae. "Water Content in the Mantle Transition Zone Beneath the North Pacific Derived from the Electrical Conductivity Anomaly." In Earth's Deep Water Cycle, 171–79. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/168gm13.

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V. Grushevskaya, Halina, and George Krylov. "Anomalous Charge Transport Properties and Band Flattening in Graphene: A Quasi-Relativistic Tight-Binding Study of Pseudo-Majorana States." In Graphene - Recent Advances, Future Perspective and Applied Applications [Working Title]. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.106144.

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Anomalous charge carrier transport in graphene is studied within a topologically nontrivial quasi-relativistic graphene model. The model predicts additional topological contributions, such as the Majorana-like mass-term correction to the ordinary ohmic component of the current, the spin-orbital-coupling, “Zitterbewegung”-effect corrections to conductivity in space, and time dispersion regime. The corrections appear due to non-Abelian quantum statistics for the charge carriers in graphene. The chiral anomaly of electrophysical and optical properties may emerge due to a deconfinement of the pseudo-Majorana quasiparticles. It has been shown that phenomena of negative differential conductivity, loss of universal far-infrared optical conductivity, and nonzero “minimal” direct-current conductivity in graphene occur due to flattening and vorticity of the pseudo-Majorana model graphene energy bands.
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LILLEY, F. E. M., L. J. WANG, F. H. CHAMALAUN, and I. J. FERGUSON. "Carpentaria Electrical Conductivity Anomaly, Queensland, as a major structure in the Australian Plate." In Evolution and Dynamics of the Australian Plate. Geological Society of America, 2003. http://dx.doi.org/10.1130/0-8137-2372-8.141.

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Conference papers on the topic "Conductivity anomaly"

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Rokityansky, I. I., and A. V. Tereshyn. "Donbas Electrical Conductivity Anomaly." In 16th International Conference Monitoring of Geological Processes and Ecological Condition of the Environment. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.2022580254.

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Chen, Chow‐Son, C. C. Chen, and C. S. Chou. "The preliminary crustal conductivity anomaly from MT data in Taiwan." In SEG Technical Program Expanded Abstracts 1996. Society of Exploration Geophysicists, 1996. http://dx.doi.org/10.1190/1.1826621.

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Vero, L., A. Madarasi, W. Seiberl, and G. Varga. "Magnetotelluric tracing of the Carpathian conductivity anomaly in the Vienna Basin." In 58th EAEG Meeting. Netherlands: EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201408667.

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Bartel, L. C., and G. A. Newman. "Mapping a 3‐D conductivity anomaly using a vertical electric source: Field results." In SEG Technical Program Expanded Abstracts 1991. Society of Exploration Geophysicists, 1991. http://dx.doi.org/10.1190/1.1889143.

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Tyurin, V., O. Bakhovskaya, M. Bakhovskaya, V. Domakhina, A. Kokh, and O. Maslovskaya. "FEATURES OF SPATIAL ASSESSMENT OF SALT POLLUTION USING A CONDUCTIVITY METER (BOG IN SURGUT LOWLAND, WESTERN SIBERIA)." In Prirodopol'zovanie i ohrana prirody: Ohrana pamjatnikov prirody, biologicheskogo i landshaftnogo raznoobrazija Tomskogo Priob'ja i drugih regionov Rossii. Izdatel'stvo Tomskogo gosudarstvennogo universiteta, 2020. http://dx.doi.org/10.17223/978-5-94621-954-9-2020-57.

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The data on electrical conductivity in a place of pollution with produced water is presented. The 2019 data reflected a physicochemical anomaly remaining 15 years after an accident. The contour of pollution is also confirmed by other signs and manifested in pH and vegetation, also displayed in satellite images.
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Kis, M., T. Bodoky, I. Kummer, and L. Sores. "Investigation of the telluric conductivity anomaly at Magyarmecske: the first assumed buried impact crater in Hungary." In 5th Congress of Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.126.6245.

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Weckmann, U., A. Jung, T. Branch, K. Tietze, and O. Ritter. "Electrical conductivity anomalies in the Namaqua Natal Mobile Belt and the Beattie magnetic anomaly: Do they have a common source?" In 10th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609-pdb.146.6.5.

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Jones, Alan G., Jon Katsube, and Ian Ferguson. "Paleoproterozoic tectonic processes revealed through electromagnetic studies of the North American Central Plains (NACP) conductivity anomaly: From continental to hand sample scale." In SEG Technical Program Expanded Abstracts 1996. Society of Exploration Geophysicists, 1996. http://dx.doi.org/10.1190/1.1826616.

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Rokityansky, I. I., E. Yu Sokolova, N. S. Golubtsova, and S. Kovachikova. "Magnetovariational studies of Lake Ladoga crustal conductivity anomaly: from discovery in 70th to understanding of its spatial behaviour and deep structure on modern observations." In 17th International Conference on Geoinformatics - Theoretical and Applied Aspects. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201801753.

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Sanin, S. S., A. A. Voronin, A. V. Kirichek, V. I. Kuznetsov, and Yu N. Dolgikh. "Test Results of Integrated Interpretation Technology of Geological-Geophysical and Field Data for the Purposes of Fracture Zones Prediction and Evaluation of The Rupture Anomaly Conductivity by Scattered Waves." In Tyumen 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202150082.

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