Relevant bibliographies by topics / Aeromagnetics

Academic literature on the topic 'Aeromagnetics'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Aeromagnetics"

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Gunn, Peter. "Aeromagnetics locates prospective areasandprospects." Leading Edge 17, no. 1 (January 1998): 67–69. http://dx.doi.org/10.1190/1.1437828.

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Rigoti, Augustinho, Antonio L. Padilha, F. H. Chamalaun, and Nalin B. Trivedi. "Effects of the equatorial electrojet on aeromagnetic data acquisition." GEOPHYSICS 65, no. 2 (March 2000): 553–58. http://dx.doi.org/10.1190/1.1444750.

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In recent years, considerable advances have taken place in aeromagnetic surveying. These improvements involved data acquisition (instruments and survey design), processing, and interpretation. In addition to improved spatial resolution, the high‐resolution aeromagnetics, as applied to oil exploration, attempts to resolve very low amplitude (1 nT or even subnanotesla) magnetic features (Paterson and Reeves, 1985). These features are caused by weak intra‐sedimentary magnetic sources of magnetite and pyrrhotite, which could have been formed as a result of hydrocarbon seepage (e.g., Reynolds et al., 1990, 1991). For such small spatial variations to be meaningful, it is required that similar temporal and spatial variations due to external sources be corrected accordingly.
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Withers, Robert, Dwight Eggers, Thomas Fox, and Terry J. Crebs. "Reply by the authors to N. C. Steenland." GEOPHYSICS 61, no. 3 (May 1996): 915. http://dx.doi.org/10.1190/1.1487023.

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The comments made by N. C. Steenland address issues of the aeromagnetic interpretation and gravity data inconsistencies. These comments will be addressed individually. The authors are very familiar with the method of aeromagnetic exploration having used it in various countries, geologic environments and applications. The technique is extremely powerful when used appropriately, and magnetics were not discounted summarily. In any paper on exploration we believe it is important that all results be discussed, and a worse disservice to the industry would have been to ignore aeromagnetics. Indeed, we would have expected criticism had we not reported on our findings about the applicability of magnetics on the Columbia River Basalts (CRB). It is our experience that working with other basalts of different ages and sources, such as the Snake River Basalt example discussed by the reviewer, may not be a guarantee of obtaining appropriate interpretations elsewhere.
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Komolafe, Akinola Adesuji, Zacharia Njuguna Kuria, Tsehaie Woldai, Marleen Noomen, and Adeleye Yekini Biodun Anifowose. "Integrated Remote Sensing and Geophysical Investigations of the Geodynamic Activities at Lake Magadi, Southern Kenyan Rift." International Journal of Geophysics 2012 (2012): 1–15. http://dx.doi.org/10.1155/2012/318301.

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The tectonic lineaments and thermal structure of Lake Magadi, southern Kenyan rift system, were investigated using ASTER data and geophysical methods. Five N-S faults close to known hot springs were identified for geoelectric ground investigation. Aeromagnetic data were employed to further probe faults at greater depths and determine the Curie-point depth. Results indicate a funnel-shaped fluid-filled (mostly saline hydrothermal) zone with relatively low resistivity values of less than 1 Ω-m, separated by resistive structures to the west and east, to a depth of 75 m along the resistivity profiles. There was evidence of saline hydrothermal fluid flow toward the surface through the fault splays. The observed faults extend from the surface to a depth of 7.5 km and are probably the ones that bound the graben laterally. They serve as major conduits for the upward heat flux in the study area. The aeromagnetics spectral analysis also revealed heat source emplacement at a depth of about 12 km. The relative shallowness implies a high geothermal gradient evidenced in the surface manifestations of hot springs along the lake margins. Correlation of the heat source with the hypocenters showed that the seismogenetic zone exists directly above the magmatic intrusion, forming the commencement of geodynamic activities.
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Grant, F. S. "Aeromagnetics, geology and ore environments, II. Magnetite and ore environments." Geoexploration 23, no. 3 (September 1985): 335–62. http://dx.doi.org/10.1016/0016-7142(85)90002-x.

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Nathan, D., A. Aitken, E. J. Holden, and J. Wong. "Imaging sedimentary basins from high-resolution aeromagnetics and texture analysis." Computers & Geosciences 136 (March 2020): 104396. http://dx.doi.org/10.1016/j.cageo.2019.104396.

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Tarlowski, C., and I. Koch. "On the problem of estimating the depth to the magnetic basement." GEOPHYSICS 53, no. 10 (October 1988): 1362–63. http://dx.doi.org/10.1190/1.1442415.

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In many applications in aeromagnetics, the estimation of the depth to the crystalline magnetic basement is of great importance. Of many approaches to this problem, the most widely applied appear to be based upon Fourier analysis (see Ruotoistenmäki, 1987) or on fitting hypothetical models to observed data using a least‐squares principle (for example, Leite and Leão, 1985). Recently, some interest has been focused on direct approaches to the problem (Strakhov and Brodsky, 1986; Koch and Tarlowski, 1986; and Jonca and Vogel, 1987).
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Heath, D. H., V. S. Clarke, and A. N. Bint. "High Resolution Aeromagnetics Clarifies Structuring in the Vlaming Sub-Basin, Western Australia." Exploration Geophysics 24, no. 3-4 (September 1993): 535–41. http://dx.doi.org/10.1071/eg993535.

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Kuras, Agnieszka, Björn H. Heincke, Sara Salehi, Christian Mielke, Nicole Köllner, Christian Rogass, Uwe Altenberger, and Ingunn Burud. "Integration of Hyperspectral and Magnetic Data for Geological Characterization of the Niaqornarssuit Ultramafic Complex in West-Greenland." Remote Sensing 14, no. 19 (September 29, 2022): 4877. http://dx.doi.org/10.3390/rs14194877.

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The integration of imaging spectroscopy and aeromagnetics provides a cost-effective and promising way to extend the initial analysis of a mineral deposit. While imaging spectroscopy retrieves surface spectral information, magnetic responses are used to determine magnetization at both shallower and greater depths using 2D and 3D modeling. Integration of imaging spectroscopy and magnetics improves upon knowledge concerning lithology with magnetic properties, enhances understanding of the geological origin of magnetic anomalies, and is a promising approach for analyzing a prospective area for minerals having a high iron-bearing content. To combine iron diagnostic information from airborne hyperspectral and magnetic data, we (a) used an iron absorption feature ratio to model pseudo-magnetic responses and compare them with the measured magnetic data and (b) estimated the apparent susceptibility along the surface by some equivalent source modeling, and compared them with iron ratios along the surface. For this analysis, a Modified Iron Feature Depth index was developed and compared to the surface geochemistry of the rock samples in order to validate the spectral information of iron. The comparison revealed a linear increase in iron absorption feature depths with iron content. The analysis was performed by empirically modeling the statistical relationship between the diagnostic absorption features of hyperspectral (HS) image spectra of selected rock samples and their corresponding geochemistry. Our results clearly show a link between the spectral absorption features and the magnetic response from iron-bearing ultra/-mafic rocks. The iron absorption feature ratio of 𝐹𝑒3+/𝐹𝑒2+ integrated with aeromagnetic data (residual magnetic anomaly) allowed us to distinguish main rock types based on physical properties. This separation matches the lithology of the Niaqornarssuit complex, our study area in West Greenland.
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Roy Chowdhury, Priyanka, Darcy Christian, Keith Jones, Warwick Crowe, and Roger Miller. "Aeromagnetics assists Oil & Gas exploration in the Bedout Sub-basin, offshore Canning Basin." ASEG Extended Abstracts 2012, no. 1 (December 2012): 1–4. http://dx.doi.org/10.1071/aseg2012ab280.

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Dissertations / Theses on the topic "Aeromagnetics"

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Bontenakel, Alexander P. "Three dimensional modelling of the Truro-Sandleton area using aeromagnetics and gravity /." Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bb722.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1993.
On title page: "National Grid reference: Adelaide sheet S1 54-9 (1:250 000). Map in pocket inside back cover. Includes bibliographical references (leaves 23-25).
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Sahu, Bijay Kumar. "Aeromagnetics of selected continental areas flanking the Indian Ocean : with implications for geological correlation and reassembly of Central Gondwana." Doctoral thesis, University of Cape Town, 2000. http://hdl.handle.net/11427/10718.

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Reassembling continental fragments of Gondwana has been a subject of interest to many since almost the beginning of the last century. As a result, the broad relative position of the major continental fragments and their dispersal history is well understood using marine magnetic anomalies, coastline geometry, surface geology and limited geophysics. Uncertainty still prevails in reassembly of central Gondwana fragments flanking the Indian Ocean. This thesis aims at utilising geophysical constraints to corroborate an fine-tune the reconstruction of these fragments supported by geological evidence.
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Thomson, G. F. "Palaeomagnetic and aeromagnetic studies of some sulphide deposits." Thesis, University of Newcastle Upon Tyne, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383983.

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Whiting, Thomas H. "A study of the lithology and structure of the eastern Arunta Inlier based on aeromagnetic interpretation : a lithological subdivision and structural history of the eastern Arunta Inlier, with particular emphasis on the relationship between magnetic mineral petrogenesis, rock magnetism and aeromagnetic signature /." Title page, contents and abstract only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phw6125.pdf.

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Casto, Daniel W. "Calculating depths to shallow magnetic sources using aeromagnetic data from the Tucson Basin." Tucson, Ariz. : U.S. Dept. of the Interior, U.S. Geological Survey, 2001. http://geopubs.wr.usgs.gov/open-file/of01-505/.

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Naudé, Corus. "Target selection from airborne magnetic and radiometric data in Steinhausen area, Namibia." Thesis, Rhodes University, 2012. http://hdl.handle.net/10962/d1001520.

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The eastern branch of the late Proterozoic Damara Orogenic Belt of central Namibia hosts various copper, gold, manganese and uranium deposits, but in the vicinity of Steinhausen, approximately 145 km northeast of Windhoek, the Damara Belt becomes increasingly covered by recent Kalahari cover sediments resulting in little known geology and subsequent lack of discovered economic mineral deposits. Airborne magnetic and radiometric data over the Steinhausen Study Area was enhanced through image processing and filtering to accentuate characteristics of subsurface geology that, by comparing these characteristics to known geology, aided in the interpretive mapping of lithology, structure and targets for follow-up exploration. As a result, some important observations regarding the regional lithology can be drawn. An arenaceous stratigraphic unit that includes a coarse grained, glassy quartzite below the Kuiseb Formation equates to either the eastern Damaran equivalent of the Nosib Group subjected to high grade metamorphism or, alternatively, the upper part of the pre-Damaran sequence, immediately underlying the Damara. The Kuiseb Formation within the study area is uncharacteristically varied as compared to the same formation further west along the Damaran Orogen and can be subdivided into 5 separate units based on geophysical signature. Structural features evident within the study area include the prominent Kudu and Okahandja Lineaments and straddle an area of inferred uplifted stratigraphy of possibly pre-Damara age. The Ekuja Dome (Kibaran age and host to the Omitiomire copper deposit) is also clearly discernible on the airborne magnetic data and is cross-cut by an east-northeast structural zone. Direct targets for follow-up exploration include the Rodenbeck intrusion, anomalous magnetic bodies and numerous radiometric anomalies present within the study area. Identified dome-like features are considered prospective for Omitiomire-style deposits and the Okatjuru Layered Complex is considered a possible source of copper, chromite, magnetite, ilmenite, nickel and the platinum group elements.
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Johnson, Ashley Charles. "A geophysical investigation of crustal structure and segmentation of the central Antarctic Peninsula." Thesis, Open University, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266417.

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Garrett, S. W. "Interpretation of regional gravity and aeromagnetic surveys of the Antarctic Peninsula." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.373905.

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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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Magaia, Luis. "Processing Techniques of Aeromagnetic Data. Case Studies from the Precambrian of Mozambique." Thesis, Uppsala universitet, Geofysik, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-183714.

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During 2002-2006 geological field work were carried out in Mozambique. The purpose was to check the preliminary geological interpretations and also to resolve the problems that arose during the compilation of preliminary geological maps and collect samples for laboratory studies. In parallel, airborne geophysical data were collected in many parts of the country to support the geological interpretation and compilation of geophysical maps. In the present work the aeromagnetic data collected in 2004 and 2005 in two small areas northwest of Niassa province and another one in eastern part of Tete province is analysed using GeosoftTM. The processing of aeromagnetic data began with the removal of diurnal variations and corrections for IGRF model of the Earth in the data set. The study of the effect of height variations on recorded magnetic field, levelling and interpolation techniques were also studied. La Porte interpolation showed to be a good tool for interpolation of aeromagnetic data using measured horizontal gradient. Depth estimation techniques are also used to obtain semi-quantitative interpretation of geological bodies. It was showed that many features in the study areas are located at shallow depth (less than 500 m) and few geological features are located at depths greater than 1000 m. This interpretation could be used to draw conclusions about the geology or be incorporated into further investigations in these areas.
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Books on the topic "Aeromagnetics"

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Dept, Malawi Geological Survey. Aeromagnetic map. [Zomba, Malawi]: The Department, 1986.

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U.S. Geological Survey Workshop on Geologic Applications of Modern Aeromagnetic Surveys (1987 Lakewood, Colo.). Geologic applications of modern aeromagnetic surveys: Proceedings of the U.S. Geological Survey Workshop on Geologic Applications of Modern Aeromagnetic Surveys, held January 6-8, 1987, in Lakewood, Colorado. Washington: U.S. G.P.O., 1990.

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Denith, M. Texture-based enhancement and classification of aeromagnetic data. East Perth, WA: Minerals and Energy Research Institute of Western Australia, 2002.

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

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Geological Survey (U.S.), ed. Principal facts for gravity data collected in Wisconsin: A web site and CD-ROM for distribution of data. [Reston, Va.]: U.S. Geological Survey, 2004.

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Gómez, Sergio Chávez. A catalogue of dykes from aeromagnetic surveys in eastern and southern Africa. Enschede, Netherlands: International Institute for Aerospace Survey and Earth Sciences, 2001.

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W, Buhmann Ronald, Racey Stewart D, and National Geophysical Data Center, eds. Project Magnet: Aeromagnetic surveys, 1953-1994 : CD-ROM user's manual. [Boulder, Colo.]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Geophysical Data Center, 1996.

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Kleinkopf, M. Dean. Aeromagnetic and gravity studies of Payette National Forest, Idaho. [Denver, CO]: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Renner, R. G. B. Reconnaissance gravity and aeromagnetic surveys of the Antarctic Peninsula. Cambridge: British Antarctic Survey, 1985.

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Dieter, Eberle, Hutchins D. G, and Geological Survey (Namibia), eds. Proceedings of the Mineral Prospecting Promotion Workshop, 1997. Windhoek, Namibia: Ministry of Mines and Energy, Geological Survey of Namibia, 2005.

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Book chapters on the topic "Aeromagnetics"

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Tedesco, Steven A. "THE USE OF AEROMAGNETICS AND MICROMAGNETICS TO IDENTIFY POTENTIAL AREAS OF HYDROCARBONS IN THE MIDCONTINENTAL UNITED STATES." In Oil and Gas Exploration, 259–75. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119227519.ch16.

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Zhou, Wendy. "Aeromagnetic Survey." In Selective Neck Dissection for Oral Cancer, 1–6. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-12127-7_8-1.

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Zhou, Wendy. "Aeromagnetic Survey." In Encyclopedia of Earth Sciences Series, 13–18. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73568-9_8.

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Hamoudi, Mohamed, Yoann Quesnel, Jérôme Dyment, and Vincent Lesur. "Aeromagnetic and Marine Measurements." In Geomagnetic Observations and Models, 57–103. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9858-0_4.

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Hinze, William J., Norbert W. O'Hara, James W. Trow, and George B. Secor. "Aeromagnetic Studies of Eastern Lake Superior." In The Earth Beneath the Continents, 95–110. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm010p0095.

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Patenaude, Robert W. "A Regional Aeromagnetic Survey of Wisconsin." In The Earth Beneath the Continents, 111–26. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm010p0111.

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Bansal, A. R., V. P. Dimri, Raj Kumar, and S. P. Anand. "Curie Depth Estimation from Aeromagnetic for Fractal Distribution of Sources." In Fractal Solutions for Understanding Complex Systems in Earth Sciences, 19–31. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-24675-8_2.

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Abraham, Ema M., and Onyekachi E. Itumoh. "Geothermal Reconnaissance of Southeastern Nigeria from Analysis of Aeromagnetic Data." In On Significant Applications of Geophysical Methods, 43–46. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01656-2_9.

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Zietz, Isidore. "Aeromagnetic Investigations of the Earth's Crust in the United States." In The Earth's Crust and Upper Mantle, 404–15. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0404.

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Wold, Richard J., and Ned A. Ostenso. "Aeromagnetic, Gravity, and Sub-Bottom Profiling Studies in Western Lake Superior." In The Earth Beneath the Continents, 66–95. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm010p0066.

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Conference papers on the topic "Aeromagnetics"

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Petzke, M., P. Hofmeister, A. Hördt, K. H. Glaßmeier, and H. U. Auster. "Aeromagnetics with an Unmanned Airship." In Near Surface Geoscience 2013. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20131321.

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Grow*, Timothy J., Fred Dula, Chris Mazis, Tim Seeley, and Melinda Sisk. "Analysis of high resolution aeromagnetics in Central California." In SEG Technical Program Expanded Abstracts 2014. Society of Exploration Geophysicists, 2014. http://dx.doi.org/10.1190/segam2014-0229.1.

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McConnell, T. J., and Z. Berger. "Sedimentary AeroMagnetics (SAM). An evaluation of Geological mapping capabilities." In 4th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609-pdb.313.71.

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Jamal, D. L., B. K. Sahu, and M. J. de Wit. "Tectonic Blocks of Northern Mozambique: Integrating Geochronology and Aeromagnetics." In 7th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.143.4.1.

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Adamson, Mackenzie. "LOCATING ABANDONED OIL AND GAS WELLS USING DRONE-AEROMAGNETICS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286813.

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McConnell, Terence J. "North Slope, Alaska: A case study of Sedimentary aeromagnetics." In SEG Technical Program Expanded Abstracts 1995. Society of Exploration Geophysicists, 1995. http://dx.doi.org/10.1190/1.1887573.

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Pridmore, D. F. "New developments in high‐resolution aeromagnetics applied to structural mapping in petroleum exploration." In SEG Technical Program Expanded Abstracts 1990. Society of Exploration Geophysicists, 1990. http://dx.doi.org/10.1190/1.1890125.

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Reid, A., H. Elstad, C. Lewis, and R. Morgan. "High sensitivity aeromagnetics from the Vøring Basin, offshore Norway - A Seismologists guid to fault linking." In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201409912.

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Tedesco, Steven. "Utilizing aeromagnetics and micromagnetics to define petroleum reservoirs in the Denver, forest city and Cherokee basins." In International Conference and Exhibition, Barcelona, Spain, 3-6 April 2016. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2016. http://dx.doi.org/10.1190/ice2016-6492540.1.

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Misener, D. James, Michael Biryabarema, and Sally Barritt. "Mineral potential of Rwanda: Prospective target areas at depth as interpreted from airborne gravity and aeromagnetics." In GEM Beijing 2011, edited by Xiong Li, Yaoguo Li, and Xiaohong Meng. Society of Exploration Geophysicists, 2011. http://dx.doi.org/10.1190/1.3659068.

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Reports on the topic "Aeromagnetics"

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Pilkington, M., F. Dostaler, and D. Oneschuk. Aeromagnetics and gravity. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/223377.

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Keating, P. Kimberlites and aeromagnetics. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/211817.

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Hayward, N., and J. J. Ryan. Geophysical characteristics of the northern Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326069.

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Geophysical data acquired under the Geological Survey of Canada's GEM Cordillera project provide a foundation to a broad range of geological investigations in the northern Canadian Cordillera. For areas of specific geological interest, over 230 000 km of high-resolution aeromagnetic data form a mosaic of comprehensive coverage over a total area of more than 82 000 km2. The data provide a powerful and valuable legacy data set for current and future activities by the Geological Survey of Canada and academic and industry partners and clients. Foremost, geophysical data interpretation complements surface geological mapping, especially in inaccessible terrain where bedrock exposure is commonly poor, enabling clearer definition of a region's geology and structure. Beyond applications to bedrock geological mapping, geophysical modelling, integrated with geological results, affords an improved understanding of the deeper crustal structure, leading to new models of the region's tectonic development and mineral deposit context.
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Pilkington, M., and D. Oneschuk. Aeromagnetic and gravity. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/223360.

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Tschirhart, V., S. Pehrsson, N. Wodicka, J. A. Percival, C. W. Jefferson, T. Peterson, and R G Berman. Geophysical contributions to a synthesis of western Churchill geology and metallogeny. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330639.

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The geophysical data sets available for the western Churchill Province have had a bearing on the understanding of its structure, evolution and metal endowment. New data were acquired and interpreted during the Geo-mapping for Energy and Minerals (GEM) Program (2008-2020). Regional, high-resolution aeromagnetic, and targeted gravity and magnetotelluric surveys were collected in GEM, in conjunction with geological mapping projects, in order to provide control on bedrock features beneath widespread glacial overburden and flat-lying sedimentary basins. Quantitative estimates of three-dimensional geometry were obtained in key areas through geophysical models integrating the geophysical characteristics with local rock property measurements. These geophysical data sets contributed to new knowledge and interpretations in three related research fields: 1) location and nature of Rae cratonmp;gt;'s boundaries within the western Churchill Province; 2) definition of internal Rae architecture; and 3) identification of reactivated structures controlling gold and uranium mineralization. The new data, models and emerging tectonic and metallogenic frameworks will serve as guides for future exploration in this remote, complex, challenging region.
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Kiss, F. Morewood Ontario aeromagnetic calibration range. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/297428.

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7

Teskey, D. J. Statistical interpretation of aeromagnetic data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128046.

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8

Tod, J., and M. Pilkington. Regional Aeromagnetic Surveys in B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131235.

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9

Keating, P., J. Tod, and R. Dumont. The National Aeromagnetic Data Base. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/211816.

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10

Macnab, R. Aeromagnetic Profiles Northeast of Orphan Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/130573.

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