Gotowe bibliografie tematyczne / Crustal anomalies

Spis treści

  1. Artykuły w czasopismach
  2. Rozprawy doktorskie
  3. Książki
  4. Części książek
  5. Streszczenia konferencji

Gotowa bibliografia na temat „Crustal anomalies”

Autor: Grafiati
Data publikacji: 6 września 2023

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Artykuły w czasopismach na temat "Crustal anomalies"

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Raymond, Carol A., and Richard J. Blakely. "Crustal magnetic anomalies." Reviews of Geophysics 33 (1995): 177. http://dx.doi.org/10.1029/95rg00444.

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Filho, Nelson Ribeiro, Cristiano Mendel Martins, and Renata de Sena Santos. "A NOVEL REGIONAL-RESIDUAL SEPARATION APPROACH FOR GRAVITY DATA THROUGH CRUSTAL MODELING." Revista Brasileira de Geofísica 36, no. 4 (2018): 1. http://dx.doi.org/10.22564/rbgf.v36i4.1980.

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ABSTRACT. Gravity anomalies normally contain information of all sources beneath Earth’s surface. Once residual anomalies exhibit information about the main target, the knowledge of this specific residual signal is extremely important to interpretation. To find this signal, it’s necessary to perform regional-residual separation. We present here a new approach of separation by using gravity crustal modeling. We divide the surface in prisms, with density given by GEMMA. We calculate the regional signal, assuming Earth’s crust can be the source of observed anomaly. This methodology was applied on
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Phillips, Jeffrey D., Richard L. Reynolds, and Herbert Frey. "CRUSTAL STRUCTURE INTERPRETED FROM MAGNETIC ANOMALIES." Reviews of Geophysics 29, S1 (1991): 416–27. http://dx.doi.org/10.1002/rog.1991.29.s1.416.

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Zheng, Shuo, Kai Qin, Lixin Wu, Yanfei An, Qifeng Yin, and Chunkit Lai. "Hydrothermal anomalies of the Earth's surface and crustal seismicity related to Ms8.0 Wenchuan EQ." Natural Hazards 104, no. 3 (2020): 2097–114. http://dx.doi.org/10.1007/s11069-020-04263-7.

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Abstract Hydrothermal anomalies related to the Ms8.0 Wenchuan earthquake (EQ) on May 12, 2009, have been widely reported. However, the reported anomalies have not been associated with multi-geosphere analysis, and space–time analysis with crustal seismicity is lacking. In this paper, the space–time variation of hydrothermal parameters, including soil moisture, soil temperature, near-surface relative humidity (RHsig995) and air temperature (TMPsfc), was first extracted and analyzed with the NCEP-FNL reanalysis dataset. The b-value (a seismic parameter from the Gutenberg–Richter law) was calcula
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Tang, Ming, Wei-Qiang Ji, Xu Chu, Anbin Wu, and Chen Chen. "Reconstructing crustal thickness evolution from europium anomalies in detrital zircons." Geology 49, no. 1 (2020): 76–80. http://dx.doi.org/10.1130/g47745.1.

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Abstract A new data compilation shows that in intermediate to felsic rocks, zircon Eu/Eu* [chondrite normalized Eu/ ] correlates with whole rock La/Yb, which has been be used to infer crustal thickness. The resultant positive correlation between zircon Eu/Eu* and crustal thickness can be explained by two processes favored during high-pressure differentiation: (1) supression of plagioclase and (2) endogenic oxidation of Eu2+ due to garnet fractionation. Here we calibrate a crustal thickness proxy based on Eu anomalies in zircons. The Eu/Eu*-in-zircon proxy makes it possible to reconstruct crust
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Oran, Rona, Benjamin P. Weiss, Yuri Shprits, Katarina Miljković, and Gábor Tóth. "Was the moon magnetized by impact plasmas?" Science Advances 6, no. 40 (2020): eabb1475. http://dx.doi.org/10.1126/sciadv.abb1475.

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The crusts of the Moon, Mercury, and many meteorite parent bodies are magnetized. Although the magnetizing field is commonly attributed to that of an ancient core dynamo, a longstanding hypothesized alternative is amplification of the interplanetary magnetic field and induced crustal field by plasmas generated by meteoroid impacts. Here, we use magnetohydrodynamic and impact simulations and analytic relationships to demonstrate that although impact plasmas can transiently enhance the field inside the Moon, the resulting fields are at least three orders of magnitude too weak to explain lunar cr
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Zheng, Ying, and Jafar Arkani-Hamed. "Joint inversion of gravity and magnetic anomalies of eastern Canada." Canadian Journal of Earth Sciences 35, no. 7 (1998): 832–53. http://dx.doi.org/10.1139/e98-035.

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The power spectra and degree correlation of the surface topography and free-air gravity anomalies of eastern Canada show that the gravity anomalies are subdivided into three parts. The short-wavelength components (30-170 km, shorter than 30 km are not well resolved) largely arise from density perturbations in the crust and to a lesser extent from the surface topography and Moho undulation, whereas the contribution of intracrustal sources to the intermediate-wavelength components (170-385 km) is comparable with that of the topography. The long-wavelength components (385-1536 km) are overcompens
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Saleh, Salah, Oya Pamukçu, and Ladislav Brimich. "The major tectonic boundaries of the Northern Red Sea rift, Egypt derived from geophysical data analysis." Contributions to Geophysics and Geodesy 47, no. 3 (2017): 149–99. http://dx.doi.org/10.1515/congeo-2017-0010.

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AbstractIn the present study, we have attempted to map the plate boundary between Arabia and Africa at the Northern Red Sea rift region including the Suez rift, Gulf of Aqaba-Dead Sea transform and southeastern Mediterranean region by using gravity data analysis. In the boundary analysis method which was used; low-pass filtered gravity anomalies of the Northern Red Sea rift region were computed. Different crustal types and thicknesses, sediment thicknesses and different heat flow anomalies were evaluated. According to the results, there are six subzones (crustal blocks) separated from each oth
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Halekas, J. S., D. A. Brain, R. P. Lin, and D. L. Mitchell. "Solar wind interaction with lunar crustal magnetic anomalies." Advances in Space Research 41, no. 8 (2008): 1319–24. http://dx.doi.org/10.1016/j.asr.2007.04.003.

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Riad, Samir, and Hassan A. El Etr. "Bouguer anomalies and lithosphere-crustal thickness in Uganda." Journal of Geodynamics 3, no. 1-2 (1985): 169–86. http://dx.doi.org/10.1016/0264-3707(85)90027-4.

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Rozprawy doktorskie na temat "Crustal anomalies"

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Launay, Nicolas. "Propriétés d'aimantation des sources géologiques des anomalies du champ magnétique terrestre : magnétisme des roches et modélisation numérique." Thesis, Aix-Marseille, 2018. http://www.theses.fr/2018AIXM0212/document.

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Cette étude s’intéresse en premier lieu aux caractéristiques magnétiques d’échantillons de BIFs (Banded Iron Formations) en provenance de Mauritanie, où est observable la plus grande partie de l’Anomalie Magnétique Ouest Africaine (AMOA). On met en évidence des valeurs de susceptibilité magnétique allant jusqu’à 3.4 SI, et d’aimantation rémanente jusqu’à 1350 A/m, dans les BIFs. Des valeurs de rapport de Koenigsberger pour la plupart supérieures à 1 impliquent également que la rémanence devrait être prise en compte pour expliquer l’AMOA. L’effet de la pression sur les propriétés magnétiques de
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Telmat, Hamid. "Crustal structure and gravity field anomalies in Eastern Canada." Thèse, Chicoutimi : Montréal : Université du Québec à Chicoutimi ; Université du Québec à Montréal, 1998. http://theses.uqac.ca.

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Hussein, Musa Jad. "Integrated and comparative geophysical studies of crustal structure of pull-apart basins the Salton Trough and Death Valley, California regions /." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2007. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Tozer, Brook. "Crustal structure, gravity anomalies and subsidence history of the Parnaíba cratonic basin, Northeast Brazil." Thesis, University of Oxford, 2017. https://ora.ox.ac.uk/objects/uuid:90ce8bb0-e55d-4b3c-87e1-aab60084ef42.

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Cratonic basins cover more than 10% of Earth's continental surface area, yet their origin remains enigmatic. In this thesis a suite of new and legacy geophysical and geological data are integrated to constrain the origin of the Parnaíba basin, a cratonic basin in Northeast Brazil. These data include a 1400 km long, deep (20 s two-way travel time) seismic reflection profile, five +/- 110 km offset wide-angle split-spread receiver gathers, gravity anomaly, and well data. In the centre of the basin, the depth to pre-Paleozoic basement is ~ 3.3 km, a zone of midcrustal reflectivity (MCR) can be t
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Hood, L. L., A. Zakharian, J. Halekas, et al. "Initial mapping and interpretation of lunar crustal magnetic anomalies using Lunar Prospector magnetometer data." AMER GEOPHYSICAL UNION, 2001. http://hdl.handle.net/10150/624001.

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Maps of relatively strong crustal magnetic field anomalies detected at low altitudes with the magnetometer instrument on Lunar Prospector are presented. On the lunar nearside, relatively strong anomalies are mapped over the Reiner Gamma Formation on western Oceanus Procellarum and over the Rima Sirsalis rille on the southwestern border of Oceanus Procellarum. The main Rima Sirsalis anomaly does not correlate well with the rille itself but is centered over an Imbrian-aged smooth plains unit interpreted as primary or secondary basin ejecta. The stronger Reiner Gamma anomalies correlate with the
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Halekas, J. S., D. L. Mitchell, R. P. Lin, et al. "Mapping of crustal magnetic anomalies on the lunar near side by the Lunar Prospector electron reflectometer." American Geophysical Union, 2001. http://hdl.handle.net/10150/624000.

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Lunar Prospector (LP) electron reflectometer measurements show that surface fields are generally weak in the large mare basalt filled impact basins on the near side but are stronger over highland terranes, especially those lying antipodal to young large impact basins. Between the Imbrium and Nectaris basins, many anomalies correlate with the Cayley and Descartes Formations. Statistical analyses show that the most strongly magnetic nearside terranes are Cayley-type light plains, terra materials, and pre-Imbrian craters. Light plains and terrae include basin impact ejecta as a major component, s
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Leinweber, Volker Thor. "Geophysical study of the conjugate East African and East Antarctic margins." Brest, 2011. http://www.theses.fr/2011BRES2017.

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The study deals with the relative movements between Africa and Antarctica in Middle Jurassic to Lower Cretaceous times using new data from four campaigns (2006-2010). Aeromagnetic measurements in the 5W Enderby Basin clearly image the continent-ocean-transition east of the Gunnerus Ridge. Spreading anomalies are absent, pointing to a formation of the oceanic crust during Cretaceous Normal superchron times. Velocity and density modelling of two wide-angle seismic profiles across the Central Mozambique continental margin reveal continental crust, thinning seawards by 50% over a distance of ~130
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Takayama, Hiromi. "Statistical Model Analysis of the Geoelectric Field to Detect Anomalous Changes due to Crustal Activities." 京都大学 (Kyoto University), 2003. http://hdl.handle.net/2433/148604.

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Sato, Kazutoshi. "Development of a monitoring technique of anomalous crustal deformations with temporally high resolution by the application of kinematic GPS." 京都大学 (Kyoto University), 2005. http://hdl.handle.net/2433/145091.

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Rey, Denis. "Structure crustale des Alpes occidentales le long du profil ECORS-CROP d'après la sismique réflexion et le champ de pesanteur." Montpellier 2, 1989. http://www.theses.fr/1989MON20157.

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Ce travail, realise dans le cadre du programme ecors-crop alpes 1986-1987, a pour but l'etude de la structure profonde sous la chaine des alpes occidentales a l'aide de donnees gravimetriques acquises et incorporees aux leves anterieurs. Deux profils gravimetriques ont ainsi ete modelises a l'aide des contraintes apportees par les donnees sismiques. Ils ont permis la confirmation du caractere cylindrique de la chaine ainsi que le mode probable de raccourcissement qui d'opererait grace a de grands chevauchements intracrustaux. Une carte d'anomalie de bouguer sur l'ensemble de la chaine des alpe
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Książki na temat "Crustal anomalies"

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1926-, Kleinkopf M. Dean, and Geological Survey (U.S.), eds. Crustal structure of Kuwait: Constraints from gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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E, John Barbara, and Geological Survey (U.S.), eds. Crustal extension and the peak Colorado River gravity high, southern Sacramento Mountains, California: A preliminary correlation. Dept. of the Interior, U.S. Geological Survey, 1994.

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E, John Barbara, and Geological Survey (U.S.), eds. Crustal extension and the peak Colorado River gravity high, southern Sacramento Mountains, California: A preliminary correlation. Dept. of the Interior, U.S. Geological Survey, 1994.

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Sobczyk, Stanley Michael. Crustal thickness and structure of the Columbia Plateau using geophysical methods. 1994.

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Khurshid, Akbar. Crustal structure of the Sulaiman Range, Pakistan, from gravity data. 1991.

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Investigation of lunar crustal structure and isostasy: Final technical report. National Aeronautics and Space Administration, 1987.

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Soofi, Muhammad Asif. Crustal structure of the northwestern continental margin of the Indian subcontinent from gravity and magnetic data. 1991.

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Roberts, Timothy H. Gravity investigation of crustal structure in the eastern Olympic Peninsula - Puget Lowland Area, Washington. 1991.

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Zamora, Osvaldo Sánchez. Crustal structure and thermal gradients of the northern Gulf of California determined using spectral analysis of magnetic anomalies. 1988.

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Braga, Luiz F. S. Isostatic evolution and crustal structures of the Amazon continental margin determined by admittance analyses and inversion of gravity data. 1991.

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Części książek na temat "Crustal anomalies"

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Ostenso, Ned A. "Magnetic Anomalies and Crustal Structure." In The Earth's Crust and Upper Mantle. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0457.

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Ogata, Yosihiko. "Anomalies of Seismic Activity and Transient Crustal Deformations Preceding the 2005 M 7.0 Earthquake West of Fukuoka." In Seismogenesis and Earthquake Forecasting: The Frank Evison Volume II. Springer Basel, 2010. http://dx.doi.org/10.1007/978-3-0346-0500-7_17.

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Ma, Zongjin, Zhengxiang Fu, Yingzhen Zhang, Chengmin Wang, Guomin Zhang, and Defu Liu. "Crustal Deformation and Anomalous Variations of Stress." In Earthquake Prediction. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-61269-5_6.

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Malahoff, Alexander. "Gravity Anomalies Over Volcanic Regions." In The Earth's Crust and Upper Mantle. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0364.

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Kim, Hyung Rae, Luis R. Gaya-Piqué, Ralph R. B. von Frese, Patrick T. Taylor, and Jeong Woo Kim. "CHAMP Magnetic Anomalies of the Antarctic Crust." In Earth Observation with CHAMP. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-26800-6_41.

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Nagata, Takesi. "Reduction of Geomagnetic Data and Interpretation of Anomalies." In The Earth's Crust and Upper Mantle. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0391.

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Pandey, Om Prakash. "Vindhyan Basin: Anomalous Crust-Mantle Structure." In Society of Earth Scientists Series. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40597-7_5.

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Simonenko, Tatiana. "Relation of Magnetic Anomalies to Topography and Geology in the USSR." In The Earth's Crust and Upper Mantle. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0415.

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Khan, M. A. "Figure of the Earth and Mass Anomalies Defined by Satellite Orbital Perturbations." In The Earth's Crust and Upper Mantle. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0293.

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Coron, S. "Gravity Anomalies as a Function of Elevation: Some Results in Western Europe." In The Earth's Crust and Upper Mantle. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm013p0304.

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Streszczenia konferencji na temat "Crustal anomalies"

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Arkani-Hamed, J., and D. W. Strangway. "Inversion of scalar magnetic anomalies of regional scale to crustal magnetization anomalies." In 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892713.

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Chen, C. H., Y. Hobara, and R. Miyake. "Potential relationship between seismo-crustal displacement and EM anomalies." In 2014 XXXIth URSI General Assembly and Scientific Symposium (URSI GASS). IEEE, 2014. http://dx.doi.org/10.1109/ursigass.2014.6929864.

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Tang, Ming, Weiqiang Ji, Xu Chu, Anbin Wu, and Chen Chen. "Reconstructing Crustal Thickness Evolution from Eu Anomalies in Detrital Zircons." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2553.

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Zeng, Hualin, Qinghe Zhang, Yishi Li, and Jun Liu. "Fault distribution and upper crustal thickness from gravity anomalies in South China." In SEG Technical Program Expanded Abstracts 1997. Society of Exploration Geophysicists, 1997. http://dx.doi.org/10.1190/1.1885958.

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Peleli, Sophia, Maria Kouli, and Filippos Vallianatos. "Thermal anomalies and crustal deformation related to the November 26, 2019, Albania (Durrës) earthquake." In 2023 Joint Urban Remote Sensing Event (JURSE). IEEE, 2023. http://dx.doi.org/10.1109/jurse57346.2023.10144203.

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Nair, Manoj, Arnaud Chulliat, Adam Woods, et al. "Next Generation High-Definition Geomagnetic Model for Wellbore Positioning, Incorporating New Crustal Magnetic Data." In Offshore Technology Conference. OTC, 2021. http://dx.doi.org/10.4043/31044-ms.

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Abstract Magnetic wellbore positioning depends on an accurate representation of the Earth's magnetic field,where the borehole azimuth is inferred by comparing the magnetic field measured-whiledrilling (MWD) with a geomagnetic reference model. Therefore, model accuracy improvements reduce the position uncertainties. An improved high-resolution model describing the core, crustal and external components of the magnetic field is presented, and it is validated with anindependent set of measurements. Additionally, we benchmark it against other high-resolution geomagnetic models. The crustal part of
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Clark, Chris, Steven M. Reddy, Martin Hand, et al. "MICRO- TO NANOSCALE CONSTRAINTS ON THE TIMING AND CONDITIONS ASSOCIATED WITH THE FORMATION LITHOSPHERIC-SCALE CONDUCTIVITY ANOMALIES IN ANHYDROUS CRUSTAL ROCKS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324416.

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Lepland, A., A. Cremiere, S. Chand, et al. "CH4-derived Carbonate Crusts of the Barents Sea - Formation Controls and Chronology." In EAGE Shallow Anomalies Workshop. EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20147422.

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Milsom, John, Phil Roach, Chris Toland, Don Riaroh, Chris Budden, and Naoildine Houmadi. "Comoros – New Evidence and Arguments for Continental Crust." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2572434-ms.

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ABSTRACT As part of an ongoing exploration effort, approximately 4000 line-km of seismic data have recently been acquired and interpreted within the Comoros Exclusive Economic Zone (EEZ). Magnetic and gravity values were recorded along the seismic lines and have been integrated with pre-existing regional data. The combined data sets provide new constraints on the nature of the crust beneath the West Somali Basin (WSB), which was created when Africa broke away from Gondwanaland and began to move north. Despite the absence of clear sea-floor spreading magnetic anomalies or gravity anomalies defi
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Stapel, G., J. Verhoef, H. Kooi, and S. Cloetingh. "Iberian Crust Analyzed by, Residual Gravity Anomalies - Moho Prediction and Isostasy." In 59th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.131.gen1997_p108.

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