Academic literature on the topic 'Aeromagnetic Anomaly'

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Journal articles on the topic "Aeromagnetic Anomaly"

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Xia, Jianghai, Donald R. Sprowl, and Dana Adkins‐Heljeson. "Correction of topographic distortions in potential‐field data: A fast and accurate approach." GEOPHYSICS 58, no. 4 (1993): 515–23. http://dx.doi.org/10.1190/1.1443434.

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The equivalent source concept is used in the wavenumber domain to correct distortions in potential‐field data caused by topographic relief. The equivalent source distribution on a horizontal surface is determined iteratively through forward calculation of the anomaly on the topographic surface. Convergence of the solution is stable and rapid. The accuracy of the Fourier‐based approach is demonstrated by two synthetic examples. For the gravity example, the rms error between the corrected anomaly and the desired anomaly is 0.01 mGal, which is less than 0.5 percent of the maximum synthetic anomal
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Liu, Yan-Xu, Wen-Yong Li, Zhi-Yuan Liu, et al. "Occurrence Characteristics of Magnetite and Aeromagnetic Prospecting Northeast of Hebei Province." Minerals 12, no. 9 (2022): 1158. http://dx.doi.org/10.3390/min12091158.

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The occurrence characteristics of magnetite and the methods to quickly and effectively explore are important topics for ore prospecting in the new era. Taking northeast of Hebei Province of China as an example, this article aimed at an important strategic mineral of magnetite, then discussed its distribution characteristics and aeromagnetic exploration methods of it. First of all, we discuss the occurrence characteristics of sedimentary metamorphic and magmatic magnetite. Then, using the latest high-precision aeromagnetic data, combined with the geological outcrops, known iron deposits, ground
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Eaton, D., and K. Vasudevan. "Skeletonization of aeromagnetic data." GEOPHYSICS 69, no. 2 (2004): 478–88. http://dx.doi.org/10.1190/1.1707068.

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Skeletonization is a syntactic pattern‐recognition method that is applied to gridded data to produce an automatic line drawing, with an associated event catalog. Previous implementations of skeletonization have been tailored for seismic data. Here, we modify that technique to render it more suitable for other types of gridded data, with particular emphasis on aeromagnetic maps. A modification from previous schemes is the use of a two‐pass approach, to reduce the effects of an otherwise problematic directional bias that discriminates against events oriented parallel to columns of the grid. The
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Yang, Mingli, Linfu Xue, and Xiangjin Ran. "Research on the Boundary Identification Method of Concealed Geological Bodies Based on Non-seismic Geophysical Data—— Taking Benxi-Xiuyan Area as an Example." E3S Web of Conferences 261 (2021): 04021. http://dx.doi.org/10.1051/e3sconf/202126104021.

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In the process of deep geological structure research, gravity and aeromagnetic anomaly data are often used to invert the distribution law of concealed geological bodies. In order to reveal the boundaries of concealed geological bodies and divide structural divisions, this paper adopts fuzzy control simulated annealing genetic algorithm () to superimpose the gravity and aeromagnetic anomaly data in Benxi-Xiuyan area and classify the patterns, and identify the main geological body boundaries and fractures. Comparing the relationship with known geological maps, the two have a higher degree of mat
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Tarlowski, C., A. J. McEwin, C. V. Reeves, and C. E. Barton. "Dewarping the composite aeromagnetic anomaly map of Australia using control traverses and base stations." GEOPHYSICS 61, no. 3 (1996): 696–705. http://dx.doi.org/10.1190/1.1443997.

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The composite aeromagnetic anomaly map of Australia, like similar maps of other continent‐size regions, contains spurious trends, warps, and base‐level shifts. These arise from the arbitrary nature of aeromagnetic data processing methods and edge matching of disparate surveys. Corrections have been applied to the Australian map based on long aeromagnetic control traverses flown around the country in January and February 1990. The control traverses were timed to coincide with a continent‐wide magnetometer array study, thus enabling accurate corrections to be made for transient (diurnal) variati
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Zhang, Jianmin, Zhaofa Zeng, Xueyu Zhao, Jing Li, Yue Zhou, and Mingxu Gong. "Deep Mineral Exploration of the Jinchuan Cu–Ni Sulfide Deposit Based on Aeromagnetic, Gravity, and CSAMT Methods." Minerals 10, no. 2 (2020): 168. http://dx.doi.org/10.3390/min10020168.

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The exploration of deep mineral resources is an important prerequisite for meeting the continuous demand of resources. The geophysical method is one of the most effective means of exploring the deep mineral resources with a large depth and a high resolution. Based on the study of the geological background, petrophysical properties, and aeromagnetic anomaly characteristics of the Jinchuan Cu–Ni sulfide deposit, which is famous throughout the world, this paper uses the widely used gravity, aeromagnetic, and CSAMT (controlled source audio-frequency magnetotellurics) methods with a complementary r
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Dilixiati, Yixiati, Eldar Baykiev, and Jörg Ebbing. "Spectral consistency of satellite and airborne data: Application of an equivalent dipole layer for combining satellite and aeromagnetic data sets." GEOPHYSICS 87, no. 3 (2022): G71—G81. http://dx.doi.org/10.1190/geo2020-0861.1.

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We present a novel approach for the combination of aeromagnetic and satellite data applying an equivalent dipole layer and spherical harmonic (SH) expansion of the dipoles. The method involves two steps: (1) inversion for the magnetic parameters of the equivalent dipole layer and (2) conversion of the magnetic parameters into SH coefficients. With this approach, SH analysis can be used for a regional study area, and, for example, the long-wavelength range of aeromagnetic data can be replaced with satellite data. We test our approach on the third, fourth, and fifth editions of the Magnetic Anom
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Arkani-Hamed, J., D. W. Strangway, D. J. Teskey, and P. J. Hood. "Comparison of MAGSAT and low-level aeromagnetic data over the Canadian Shield: implications for GRM." Canadian Journal of Earth Sciences 22, no. 9 (1985): 1241–47. http://dx.doi.org/10.1139/e85-128.

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Band-limited magnetic anomalies over the Canadian Shield, for wavelengths of ~500–2200 km, derived from the magnetometer satellite (MAGSAT) data correlate peak for peak with the corresponding anomalies derived from the aeromagnetic data. This suggests that the anomalies detected by MAGSAT are physically meaningful. A new potential field satellite, Geopotential Research Mission (GRM), has been proposed to fly at about 160 km altitude. The magnetic anomaly map that can be derived from the GRM data is expected to have a resolution about an order of magnitude higher than the one derived from MAGSA
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Charles Ugwu Ugwueze, Nwofor, Victor Udokamma, Njoku, Ikechukwu Onyema, Jack Leah, Choko Chukwuemeka, and Ibeneme Sabinus Ikechukwu. "Qualitative Evaluation of Geophysical Aeromagnetic Data For River Anticline Around The River Niger Area In Koton-Karfi, Southern Bida Basin, Nigeria." Pacific International Journal 3, no. 2 (2020): 29–32. http://dx.doi.org/10.55014/pij.v3i2.93.

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 In this paper a qualitative evaluation of aeromagnetic data maps has been used to preliminarily support the formation of river anticlines beneath major rivers due to isostatic rebound as a result of deep river incision of surface and sub-surface overlying rocks. The regional gradients of digital high resolution aeromagnetic data were removed by polynomial fitting. This involved fitting a plane surface to the reduction to pole map of the aeromagnetic data by using multi-regression least square analysis of the Oasis Montaj 6.4 program. The regional field values from the plan
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Soto, Ruth, África Gamisel-Muzás, Concepción Ayala, et al. "Bouguer and aeromagnetic anomalies in the Iberian Chain (NE Spain); a qualitative interpretation." Geogaceta 75 (June 29, 2024): 83–86. http://dx.doi.org/10.55407/geogaceta100780.

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This work shows the Bouguer and aeromagnetic anomaly maps of the Iberian Chain (NE Spain) and surroundings in relation to its main geological and structural units. In general, both gravity and aeromagnetic anomalies are aligned following the same trends in both maps highlighting the major role played by the structural configuration of the Iberian Chain on their origin. In detail most anomalies do not coincide, pointing to different potential field sources to account for them. Further studies would be needed to decipher the origin of most magnetic anomalies observed in the Iberian Chain.
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Dissertations / Theses on the topic "Aeromagnetic Anomaly"

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Lucius, Jeffrey E. "Crustal geology of Ohio inferred from aeromagnetic and gravity anomaly analysis." The Ohio State University, 1985. http://rave.ohiolink.edu/etdc/view?acc_num=osu1318868502.

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Harvey, Leslie M. "Examination of an aeromagnetic anomaly over the Talisker Mine area on the southern Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1989. http://web4.library.adelaide.edu.au/theses/09SB/09sbh342.pdf.

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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 overlyi
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Le, Maire Pauline. "Caractérisation des anomalies magnétiques, approches théoriques et expérimentales : applications à des objets anthropiques et géologiques." Thesis, Strasbourg, 2017. http://www.theses.fr/2017STRAH006/document.

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L’objectif de ce travail est d’améliorer la caractérisation des sources à l’origine d’anomalies magnétiques, par le biais de développements théoriques et expérimentaux. Pour des structures invariantes dans une direction horizontale (structures à 2D), l’idée de Nabighian (1972) a été généralisée, ce qui implique une nouvelle façon d’étudier les méthodes potentielles à 2D. Ces développements ont permis de proposer une nouvelle approche théorique et de nouvelles représentations dans le plan complexe des fonctions magnétiques. La deuxième approche de ce travail est expérimentale. Une étude y est f
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Harvey, L. M. "Examination of an aeromagnetic anomaly over the Talisker Mine area on the southern Fleurieu Peninsula, South Australia." Thesis, 1989. http://hdl.handle.net/2440/119293.

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This item is only available electronically.<br>A N-E striking elongate aeromagnetic anomaly is observed over the Talisker Mine area, on the southern Fleurieu Peninsula, which has character and amplitude similar to an anomaly observed at Delamere (several kilometres to the north) found to be caused by magnetic Brachina Formation. Geological and geophysical techniques have been used to determine if the rock type at Talisker is also magnetic Brachina Formation, why there is a gap between the two anomalies, and why the anomaly at Talisker ends near the south coast. Geological mapping, micros
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Hansen, Cody Robert Daniel. "Magnetic signature characterization of a fixed-wing vertical take-off and landing (VTOL) unmanned aerial vehicle (UAV)." Thesis, 2018. https://dspace.library.uvic.ca//handle/1828/10413.

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The use of magnetometers combined with unmanned aerial vehicles (UAVs) is an emerging market for commercial and military applications. This study presents the methodology used to magnetically characterize a novel fixed-wing vertical take-off and landing (VTOL) UAV. The most challenging aspect of integrating magnetometers on manned or unmanned aircraft is minimizing the amount of magnetic noise generated by the aircraft’s onboard components. As magnetometer technology has improved in recent years magnetometer payloads have decreased in size. As a result, there has been an increase in opportunit
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Books on the topic "Aeromagnetic Anomaly"

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C, Jachens Robert, and Geological Survey (U.S.), eds. Preliminary aeromagnetic anomaly map of California. U.S. Geological Survey, 1999.

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McCormick, Kelli A. Drilling of an aeromagnetic anomaly in southeastern South Dakota: Results from analysis of paleozoic and precambrian core. University of South Dakota, Akeley-Lawrence Science Center, 2005.

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Bath, G. D. Investigation of an aeromagnetic anomaly on west side of Yucca Mountain, Nye County, Nevada. U.S. Dept. of the Interior, Geological Survey, 1985.

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E, Jahren Charles, United States. Dept. of Energy. Nevada Operations Office, and Geological Survey (U.S.), eds. Investigation of an aeromagnetic anomaly on west side of Yucca Mountain, Nye County, Nevada. U.S. Dept. of the Interior, Geological Survey, 1985.

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E, Jahren Charles, United States. Dept. of Energy. Nevada Operations Office., and Geological Survey (U.S.), eds. Investigation of an aeromagnetic anomaly on west side of Yucca Mountain, Nye County, Nevada. U.S. Dept. of the Interior, Geological Survey, 1985.

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Geological Survey (U.S.), ed. Aeromagnetic, Gravity Anomaly, And Derivative Maps Of The Craig And Dixon Entrance 1-Degree By 3-Degree Quadrangles Of Southeastern Alaska, U.S. Geological Survey, U.S. Geological Survey Digital Data Series DDS-56, 1999, (CD-ROM). s.n., 2000.

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Project, Nordkalott. Aeromagnetic anomaly map, northern Fennoscandia: Total intensity referred to DGRF-65. Nordkalott Project, 1986.

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Project, Mid-Norden. Aeromagnetic anomaly map of central Fennoscandia: Total intensity referred to DGRF-65. Mid-Norden Project, 1996.

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Wynn, Jeffrey C. Aeromagnetic, gravity anomaly, and derivative maps of the Craig and Dixon Entrance 1-degree by 3-degree quadrangles of southeastern Alaska. USGS Information Services (Map and Book Sales), 1999.

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Book chapters on the topic "Aeromagnetic Anomaly"

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Behrendt, John C., Anne E. McCafferty, Detlef Damaske, and Philip R. Kyle. "High Amplitude Aeromagnetic Anomaly Over the Butcher Ridge Igneous Complex: Evidence of Possible Jurassic Cumulate Rocks in the Transantarctic Mountains Bordering the Ross Embayment." In Antarctic Research Series. American Geophysical Union, 2013. http://dx.doi.org/10.1002/9781118668207.ch1.

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Behrendt, John C., Anne E. McCafferty, Detlef Damaske, and Philip R. Kyle. "High amplitude aeromagnetic anomaly over the Butcher Ridge igneous complex: Evidence of possible Jurassic cumulate rocks in the Transantarctic Mountains bordering the Ross Embayment." In Antarctic Research Series. American Geophysical Union, 1995. http://dx.doi.org/10.1029/ar067p0001.

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"aeromagnetic anomaly map." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_10853.

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Yarger, Harold L. "18. Kansas Basement Study Using Spectrally Filtered Aeromagnetic Data." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch18.

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Spector, Allan, Peter J. Hood, Abul Farah, and Waheeduddin Ahmed. "12. Applications of Aeromagnetic Data to Mineral-Resources Exploration—Baluchistan, Pakistan." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch12.

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Minghua, Zhang, and Guan Zhining. "High Resolution Curie Depth and Stratum Interface Inversion Using Aeromagnetic Anomaly." In Geophysics. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070853-14.

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Chandler, Val W. "29. Interpretation of Precambrian Geology in Minnesota Using Low-Altitude, High-Resolution Aeromagnetic Data." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch29.

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Urquhart, W. E. S., and D. W. Strangway. "32. Interpretation of Part of an Aeromagnetic Survey in the Matagami Area of Quebec." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch32.

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Cordell, Lindrith, and V. J. S. Grauch. "16. Mapping Basement Magnetization Zones from Aeromagnetic Data in the San Juan Basin, New Mexico." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch16.

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Hildenbrand, T. G., and R. P. Kucks. "19. Model of the Geothermal System in Southwestern South Dakota from Gravity and Aeromagnetic Studies." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch19.

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Conference papers on the topic "Aeromagnetic Anomaly"

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Bergeron, Luke, and Aaron Nielsen. "Aeromagnetic Anomaly Mapping for Navigation." In 2023 IEEE/ION Position, Location and Navigation Symposium (PLANS). IEEE, 2023. http://dx.doi.org/10.1109/plans53410.2023.10140125.

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Yang, Yuxin, Pengfei Zhang, Ying Shen, and Changlong Li. "An improved genetic support vector machine method for aeromagnetic anomaly detection." In International Workshop on Gravity, Electrical & Magnetic Methods and Their Applications, Shenzhen, China, May 19–22, 2024. Society of Exploration Geophysicists and Chinese Geophysical Society, 2024. http://dx.doi.org/10.1190/gem2024-073.1.

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Zhou, Jiaxin, Bo Zhang, Long Fan, and Zengquan Lu. "Aeromagnetic Anomaly Detection under Low SNR Conditions Using Multiscale Wavelet Energy Accumulation." In 2020 IEEE 20th International Conference on Communication Technology (ICCT). IEEE, 2020. http://dx.doi.org/10.1109/icct50939.2020.9295710.

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Caratori Tontini, F. "New Techniques of Geophysical Surveys Data Processing – The Aeromagnetic Anomaly Map of Italy." In 1st EAGE North African/Mediterranean Petroleum & Geosciences Conference & Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.8.t007.

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Wang, J., C. Yao, Z. Li, Q. Liu, and Y. Zheng. "Deep Structure of the Gangdese Batholith in Southern Tibet Constrained by Aeromagnetic Anomaly." In 81st EAGE Conference and Exhibition 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201901495.

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Yan, Qinghua, Shijing Zheng, Qingshan Zhang, Zhaoqiang Huang, Min Qi, and Fuzhong Xu. "Lithodemic unit identification for Huashan rock mass based on aeromagnetic anomaly boundary enhancement." In International Conference on Remote Sensing, Mapping, and Geographic Systems (RSMG 2023), edited by Feiyue Mao, Chunmei Wang, and Zhaowu Yu. SPIE, 2023. http://dx.doi.org/10.1117/12.3010293.

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Foss, C., C. Krapf, L. Katona, P. Heath, R. Dutch, and I. Gonzalez-Alvarez. "Aeromagnetic anomaly mapping of possible heavy mineral accumulations in the Coompana area of South Australia." In EAGE-GSM 2nd Asia Pacific Meeting on Near Surface Geoscience and Engineering. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201900415.

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de Oliveira, Daniel Shkromada, and Marta Silvia Maria Mantovani. "Study of Pratinha-II magnetic anomaly: Acquisition, processing and interpretation of aeromagnetic and gravimetric data." In 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15-18 August 2011. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2011. http://dx.doi.org/10.1190/sbgf2011-116.

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Araújo, Bruno, Maria da Gama, Flávio Junior, et al. "Refining Structural Interpretation by Using the Composite Map of the Vertical Derivatives of Aeromagnetic Anomaly Data." In International Congress of the Brazilian Geophysical Society&Expogef. Brazilian Geophysical Society, 2019. http://dx.doi.org/10.22564/16cisbgf2019.197.

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Yang, Mingli, Linfu Xue, Xiangjin Ran, and Haijun Wang. "A New Method for Characteristic Analysis of Gravity and Aeromagnetic Anomaly Data Based on Intelligent Clustering-FASAGA." In 2021 International Conference on Communications, Information System and Computer Engineering (CISCE). IEEE, 2021. http://dx.doi.org/10.1109/cisce52179.2021.9445942.

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Reports on the topic "Aeromagnetic Anomaly"

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Ross, G. M., J. Mariano, R. Dumont, B. A. Kjarsgaard, and D. Teskey. Was Eocene magmatism widespread in the subsurface of southern Alberta? Evidence from new aeromagnetic anomaly data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209215.

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Aeromagnetic and gravity anomaly maps of the southwestern Nevada volcanic field, Nevada and California. US Geological Survey, 1997. http://dx.doi.org/10.3133/gp1015.

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Aeromagnetic anomaly map of the Paducah 1 degree by 2 degrees Quadrangle, Missouri, Illinois, and Kentucky. US Geological Survey, 1990. http://dx.doi.org/10.3133/mf2131.

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Aeromagnetic-anomaly map and related geophysical maps of the Delta 1 degree by 2 degrees Quadrangle, Utah. US Geological Survey, 1991. http://dx.doi.org/10.3133/mf2081b.

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Gravity and aeromagnetic anomaly maps of the Ajo and Lukeville 1 degree by 2 degrees quadrangles, southwestern Arizona. US Geological Survey, 1991. http://dx.doi.org/10.3133/i2139.

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Aeromagnetic and gravity anomaly maps and a hydrothermal veins favorability map of the Wallace 1 degree by 2 degrees Quadrangle, Montana and Idaho. US Geological Survey, 1988. http://dx.doi.org/10.3133/mf1354e.

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