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Artykuły w czasopismach na temat „Euler Deconvolution and Hydrocarbon accumulation”

Autor: Grafiati

Data publikacji: 3 czerwca 2025

Data aktualizacji: 31 lipca 2025

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1

S.A, Ajala, Salako K. A, Rafiu A. A, Alahassan U. D, Adewumi T, and Sanusi Y.A. "ESTIMATION OF SEDIMENTARY THICKNESS FOR HYDROCARBON POTENTIAL OVER PART OF ADAMAWA TROUGH, NE NIGERIA USING MAGNETIC METHOD." Earth Sciences Pakistan 5, no. 1 (2021): 01–05. http://dx.doi.org/10.26480/esp.01.2021.01.05.

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This study presents the results of the analysis and interpretation of aeromagnetic data over part of Adamawa trough with the aim of investigating the hydrocarbon potential of the study area. The study area is located between latitude 8.50oN and 9.50oN and longitudes 11.50oE and 12.50oE. The Total magnetic intensity map of the study area was subjected to regional/residual separation. Three depth estimating techniques applied on the residual map to determine the thickness of sediments in the study area were Source parameter imaging, Euler deconvolution and spectral method. The results of these m

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2

Ndubuisi, Egwuonwu, Gabriel, Ibe, Stephen Onyejiuwaka, Ejike, Kingsley Nnaemeka, Orji Obinwa, and Ombu Righteous Emmanuel. "Investigation of the Gravity Anomalies within Brass and Environs, Niger Delta Area, Nigeria: Implications for Hydrocarbon Prospectivity." International Journal of Research and Innovation in Applied Science VIII, no. VI (2023): 45–56. http://dx.doi.org/10.51584/ijrias.2023.8606.

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The airborne gravity data over Brass Area and environs, Niger Delta Area, Nigeria were processed and interpreted in order to delineate the sedimentary thickness within the basin and map out places with the potentials for hydrocarbon formation, accumulation and migration. The geological structures, depths andstructural trends within the area were investigated using Total Horizontal Gradient, Tilt Derivative, Analytical Signal Filters and Euler Deconvolution techniques. The results from Euler depths showed that the sedimentary thickness and structural depths within the area range from about 1.6

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Ali, I., F. Edino, K. O. Ibrahim, I. O. Folorunso, and L. M. Johnson. "AEROMAGNETIC MAPPING OF BASINAL STRUCTURES OVER PART OF NIGER DELTA, AND ITS IMPLICATION FOR HYDROCARBON MIGRATION AND ACCUMULATION." Continental J. Earth Sciences 7, no. 1 (2012): 48–56. https://doi.org/10.5281/zenodo.833427.

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Aeromagnetic imaging over part of Niger Delta was carried out with a view to interpret the anomalies over the areand to equally delineate the structural features suitable for hydrocarbon accumulation within the study area.econd vertical derivative, first horizontal derivative and analytic signal were applied to enhance deep seated structures.The derivative maps revealed parallel to sub-parallel trending NE-SW fracture zones in the basement underlying the study area, coinciding with the landward extension of the deep oceanic Chain and Charcot fracture zones. Hence, the identified lineaments (fa

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Akor Yakubu, John, Friday Egbunu, Ngozi Agatha Okwesili, Igwe Emmanuel Awucha, and Ngozi Mariam Rita Ossai. "GEOPHYSICAL INVESTIGATION OF IWO AND ILESHA, OSUN STATE USING HIGH RESOLUTION AEROMAGNETIC DATA." Geological Behavior 7, no. 2 (2023): 69–74. http://dx.doi.org/10.26480/gbr.02.2023.69.74.

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The study deals with the Geophysical investigation of Iwo and Ilesha, Osun State, using aeromagnetic data. Qualitative as well as quantitative interpretation of the aeromagnetic data were carried out to obtain more information about the thickness of sedimentary basins. Two methods were used in the interpretation; there are Euler deconvolution method and source parameter imaging (SPI). Oasis Montaj software was employed in the analysis, the Magnetic intensity ranges from a minimum value of -22.7 nT to a maximum value of 110.4 nT, this indicate that the area is characterised with low and high ma

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Halidou Amadou, Abdourhamane, Driss El Azzab, and Abdel Ali Chaouni. "CONTRIBUTION OF AEROGRAVITY DATA INTERPRETATION TO THE STUDY OF THE DEEP STRUCTURE OF AGADEM PETROLEUM BLOCK (NIGER)." Geodesy and cartography 49, no. 3 (2023): 157–65. http://dx.doi.org/10.3846/gac.2023.17299.

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The main information provided by gravity maps is the geographical distribution of density heterogeneities in the subsurface. It is an important tool widely used for the mapping of geological structures, especially in the oil industry. Thus, this study based on the interpretation of aerogravity data has for objective, the qualitative description of the characteristics of the gravity anomalies of the study area, interpretation and mapping of the gravity lineaments as well as their depths, knowing that the lineaments constitute potential structural traps favorable to the accumulation of the hydro

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6

Essam, Aida, Abdullah Mahmoud El-Sayed, and Ahmad Sobhy Helaly. "Evaluation of tectonic trends affecting hydrocarbon accumulation of El-Obaiyed Field, Bir Fouad area, Egypt, using gravity and dipmeter data." Leading Edge 44, no. 4 (2025): 300–309. https://doi.org/10.1190/tle44040300.1.

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Bir Fouad is a significant region in the Western Desert of Egypt. It includes El-Obaiyed Field, which is considered the main Jurassic gas and condensate asset for the Shell-BAPETCO organization in the north part of the Western Desert. This field is strategically important due to its major contribution to Egypt's oil production. The purpose of the gravity data is to use disturbances in earth's gravitational field at the surface to outline the subsurface structures (faults) and determine the depth of the basement as the base of the planning area. The Bouguer gravity anomaly map was separated int

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Ibe Alexander Omenikolo, Terhemba Theophilus Emberga, and Alexander Iheanyichukwu Opara. "Basement depth re-valuation of anomalous magnetic bodies in the lower and middle Benue trough using Euler deconvolution and spectral inversion techniques." World Journal of Advanced Research and Reviews 14, no. 2 (2022): 129–45. http://dx.doi.org/10.30574/wjarr.2022.14.2.0356.

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Spectral technique and Euler Deconvolution were applied to high-resolution aeromagnetic data of parts of Benue trough to estimate the depth of anomalous magnetic sources within the study area; Data enhancement techniques such as total magnetic intensity map, reduction to pole, regional-residual separation and upward continuation maps were employed to identify different magnetic anomalies, structural trends representing the tectonics of the location were observed trending NE-SW and N-S directions; The result of 3D Euler deconvolution for the structural index (SI) = 0, 1, 2, 3 gave depths to mag

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8

Ibe, Alexander Omenikolo, Theophilus Emberga Terhemba, and Iheanyichukwu Opara Alexander. "Basement depth re-valuation of anomalous magnetic bodies in the lower and middle Benue trough using Euler deconvolution and spectral inversion techniques." World Journal of Advanced Research and Reviews 14, no. 2 (2022): 129–45. https://doi.org/10.5281/zenodo.7186181.

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Spectral technique and Euler Deconvolution were applied to high-resolution aeromagnetic data of parts of Benue trough to estimate the depth of anomalous magnetic sources within the study area; Data enhancement techniques such as total magnetic intensity map, reduction to pole, regional-residual separation and upward continuation maps were employed to identify different magnetic anomalies, structural trends representing the tectonics of the location were observed trending NE-SW and N-S directions; The result of 3D Euler deconvolution for the structural index (SI) = 0, 1, 2, 3 gave depths to mag

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9

Doğru, Fikret, and Nafiz Maden. "Hydrocarbon reservoir depth identification in the eastern black sea basin: Implications from euler deconvolution and gravity tensor invariants." Marine and Petroleum Geology 151 (May 2023): 106201. http://dx.doi.org/10.1016/j.marpetgeo.2023.106201.

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D., A. Obi, J. Ilozobhie A., E. Lebo S., and Zoogbara Evidence. "Modeling Magnetic Basement in Relationship to Hydrocarbon Habitats in the Central Niger Delta, Nigeria." Journal of Geography, Environment and Earth Science International 10, no. 4 (2017): 1–13. https://doi.org/10.9734/JGEESI/2017/31888.

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Aeromagnetics has over the years been used as a reconnaissance tool for hydrocarbon exploration. Modeling of source of magnetic anomalies can also reveal basin depth and configuration of supposed hydrocarbon habitats. This study was done using (8) aeromagnetic maps on a scale of 1:100,000 covering the central Niger Delta states in Nigeria. The data was digitized and processed using the United States Geological Survey potential field software’s version 2.2 for map merging, reduction to pole, polynomial filtering, horizontal gradient magnitude (HGM), Wenner deconvolution, forward and inverse mod

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11

Olokoba, Saheed Oluwakemi, and Yusuf Magaji. "ANALYSIS OF HIGH-RESOLUTION AEROMAGNETIC DATA OVER PARTS OF SOKOTO BASIN, NORTH-WEST NIGERIA." Platform : A Journal of Engineering 4, no. 2 (2020): 14. http://dx.doi.org/10.61762/pajevol4iss2art8601.

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Sokoto Basin is one of the sedimentary basins suspected to have high hydrocarbon potential. Hence, due to the possible deposit of this economic mineral, it is worthy of being preliminarily investigated. This paper uses high-resolution aeromagnetic data over parts of Sokoto Basin covering longitude 4.00°E-5.00°E and longitude 12.00°N-13.00°N, to assess the sedimentary thickness beneath the subsurface while also establishing the basement topography. The studied area covered four adjacent one-degree sheets, namely, sheet 27 (Lema), sheet 28 (Argungu), sheet 49 (BirninKebbi) and sheet 50 (Tambuwal

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12

Olatubosun, Esho Oluwaseyi, Osisanya Olajuwon Wasiu, Ibitoye Taiwo Abel, Ajibade Femi Zephaniah, and Tokunbo Sanmi Fagbemigun. "Aeromagnetic Interpretation of Basement Structures and Geometry in Parts of the Middle Benue Trough, North Central, Nigeria." Advances in Geological and Geotechnical Engineering Research 4, no. 4 (2022): 22. http://dx.doi.org/10.30564/agger.v4i4.5128.

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The research of an analysis of aeromagnetic data collected in the middle Benue Trough in north-central Nigeria is presented. A detailed analysis of basement structures is conducted in order to identify regions with high hydrocarbon potential that is different from those discovered by earlier researchers. Aeromagnetic data were filtered by using the Butterworth and Gaussian filters, transformed by engaging the reduction to the equator technique, and subsequently enhanced. To estimate magnetic basement depths at various places throughout the basin, the Euler deconvolution depth weighting approac

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13

Abubakar, Adamu, Othniel Kamfani Likkason, Ahmed Sadiq Maigari, and Sani Ali. "Structural Mapping Inferred from Gravity Data to Image the Upper Lithospheric Structures and its Hydrocarbon Implication from Gwandu Formation NW, Nigeria." Indonesian Journal of Earth Sciences 2, no. 1 (2022): 78–95. http://dx.doi.org/10.52562/injoes.v2i1.346.

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Presently a digitized composite satellite gravity data covering the Gwandu formation in Sokoto Basin were acquired and processed with a view to interpret the Bouguer anomalies as well to equally image the upper lithospheric structures beneath the Study area and its environs. The research work was aim to study the structural settings of crustal movement in the Gwandu formation. A least-square fitting polynomial surface of a third-degree order was applied in separating regional and residual gravity components from the Bouguer anomaly. The attributed low gravity sedimentary infill from the residu

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14

Kamto, Paul Gautier, Willy Lemotio, Alain-Pierre Kamga Tokam, and Loudi Yap. "Combination of Terrestrial and Satellite Gravity Data for the Characterization of the Southwestern Coastal Region of Cameroon: Appraisal for Hydrocarbon Exploration." International Journal of Geophysics 2021 (June 23, 2021): 1–14. http://dx.doi.org/10.1155/2021/5554528.

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The southwestern coastal region of Cameroon is an area of interest because of its hydrocarbon potential (gas and oil). Terrestrial and satellite gravity data were combined and analyzed to provide a better precision in determining the structure of the study area. Firstly, the two gravity databases (in situ and satellite) have been coupled and validated using the least square collocation technique. Then, spectral analysis was applied to the combined Bouguer anomaly map to evaluate the thickness of sediments in some localities. We found that the sedimentary cover of the southwestern coastal regio

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15

Hussaini, Adamu, and Abdullah Musa Ali. "AREAL AND DEPTH ESTIMATION OF SUBSURFACE ANOMALOUS STRUCTURES OF OYANDEGA AND ENVIRONS, PART OF THE ANAMBRA BASIN USING 2D MODELLING OF MAGNETIC DATA." Geological Behavior 8, no. 1 (2024): 90–98. https://doi.org/10.26480/gbr.02.2024.90.98.

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This study employed spectral analysis, Source Parameter Imaging (SPI), and Euler deconvulation techniques on two aeoromagnetic data sheets (Illushi 286 and Nsukka 287) to assess the depth to sub-surface structures and estimate the depth to magnetic sources at the transition region of Oyandega Area, Ibaji local government of Kogi state, part of lower Benue Trough (Anambra Basin). SPI techniques show minimum to maximum depth to anomalous source as 25.765m to 2533.293m. Euler deconvolution for contact body (Structural Index=1), indicate depth ranges from -473.70m to 751.11m, for extrusive body li

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16

GHONEIMI, Ashraf, Nashat S. GAWISH, and Muhammad NABIH. "Integrated geophysical and geochemical study for investigating the hydrocarbon potentiality of West Dakhla area, Western Desert, Egypt, as an extension of Libyan Kufra basin." Contributions to Geophysics and Geodesy 52, no. 3 (2022): 467–99. http://dx.doi.org/10.31577/congeo.2022.52.3.6.

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The present study represents an integrated study using the potential field maps and well geochemical data of the West Dakhla area in the western central area of the Western Desert area, Egypt. The potential field data are represented by the airborne gravity and total magnetic maps acquired by the Nuclear Material Authority (NMA), Egypt, on behalf of Dana Petroleum Company. The geochemical data consist of geochemical analysis in Ammonite-1 well that were done for source rock evaluation. Different processing techniques on the gravity and magnetic maps are carried out for separating the regional

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17

Lukacova, Viera, Ming Peng, Gail Fanucci, et al. "Drug-Membrane Interactions Studied in Phospholipid Monolayers Adsorbed on Nonporous Alkylated Microspheres." Journal of Biomolecular Screening 12, no. 2 (2007): 186–202. http://dx.doi.org/10.1177/1087057106297063.

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Characterization of interactions with phospholipids is an integral part of the in vitro profiling of drug candidates because of the roles the interactions play in tissue accumulation and passive diffusion. Currently used test systems may inadequately emulate the bilayer core solvation properties (immobilized artificial membranes [IAM]), suffer from potentially slow transport of some chemicals (liposomes in free or immobilized forms), and require a tedious separation (if used for free liposomes). Here the authors introduce a well-defined system overcoming these drawbacks: nonporous octadecylsil

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18

Chang, Shuai, Dalong Zhang, Linfeng Zhang, et al. "A Joint Graph-Based Approach for Simultaneous Underwater Localization and Mapping for AUV Navigation Fusing Bathymetric and Magnetic-Beacon-Observation Data." Journal of Marine Science and Engineering 12, no. 6 (2024): 954. http://dx.doi.org/10.3390/jmse12060954.

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Accurate positioning is the necessary basis for autonomous underwater vehicles (AUV) to perform safe navigation in underwater tasks, such as port environment monitoring, target search, and seabed exploration. The position estimates of underwater navigation systems usually suffer from an error accumulation problem, which makes the AUVs difficult use to perform long-term and accurate underwater tasks. Underwater simultaneous localization and mapping (SLAM) approaches based on multibeam-bathymetric data have attracted much attention for being able to obtain error-bounded position estimates. Two p

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Попков, Вячеслав Иванович, and Александр Моисеевич Штеренберг. "Post-sedimentation structure of zhiguli dislocation and neo-tectonics of cis-urals domaniks. Geological risks of development." Нефтяная провинция, no. 4(8) (December 28, 2016): 1–22. http://dx.doi.org/10.25689/np.2016.4.1-22.

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Представлена феноменологическая модель геомеханики структурирования гетерогенно-равновесной постседиментации геофизической синергии ритмов массива горных пород Жигулевской дислокации. Представлены дополнительные исследования, сейсмологи-ческая, тектонофизическая, геологическая, геофизическая информация поиска и разведки нетрадиционных месторождений и геогидродинамического моделирования этапов разработки сложнопостроенных коллекторов динамического порового пространства. Исследовано напряженно-деформированное состояние горного массива и скважин в процессе подземной разработки для крупномасштабны

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A Nwos Prisca-Gaelle, Bien, Mounchili Ibrahim, Apouamoun Yiagnigni Roland, Etoundi Jean, Ndongue Constantin, and Meying Arsene. "THE CONTRIBUTION OF REMOTE SENSING AND AEROMAGNETISM TO GOLD PROSPECTING: THE CASE OF THE MEIGANGA ZONE, CAMEROON." International Journal of Advanced Research 9, no. 5 (2021): 775–93. http://dx.doi.org/10.21474/ijar01/12903.

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In order to optimize gold prospecting in the Meiganga zone located in the Adamaoua region of Cameroon, aeromagnetic and remote sensing prospecting was carried out in the eastern and southern parts. The remote sensing approach on a Landsat 8 OLI/TIRS image highlighted areas of maximum gold concentration. Thus, ferric ion bearing minerals are located in the North-West, silicate minerals bearing ferrous ions are in the Centre while clay minerals are in the North-East and East. The principal component analysis revealed important structural information. The PCA Spatial Map (PC1, PC2, PC3) showed th

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Elawadi, Eslam, Ibraheim Gaafar, Gad El-Qady, Mohamed Metwaly, and Sándor Szalai. "Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt." Open Geosciences 16, no. 1 (2024). http://dx.doi.org/10.1515/geo-2022-0720.

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Abstract The south-eastern part of the Egyptian desert had been waiting for a long time for an exploration process of hydrocarbon potentiality. In this research, we are addressing the available high resolution airborne magnetic data of Delta Wadi Diit area, which were processed and interpreted to map the basement depths and structures as an aid for hydrocarbon potentiality elucidation. Applying a set of automatic interpretation techniques to the magnetic data enabled mapping the tectonic framework of the study area and determining the depth to the basement (in other words, thickness of sedimen

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Layade, Gideon Oluyinka, Hazeez Edunjobi, Victor Makinde, and Babatunde Bada. "Estimation of Depth to Bouguer Anomaly Sources Using Euler Deconvolution Techniques." Materials and Geoenvironment, May 3, 2021. http://dx.doi.org/10.2478/rmzmag-2020-0016.

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Abstract The geophysical measurement of variations in gravitational field of the Earth for a particular location is carried out through a gravity survey method. These variations termed anomalies can help investigate the subsurface of interest. An investigation was carried out using the airborne satellite-based (EGM08) gravity dataset to reveal the geological information inherent in a location. Qualitative analysis of the gravity dataset by filtering techniques of two-dimensional fast Fourier transform (FFT2D) shows that the area is made up of basement and sedimentary Formations. Further enhanc

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Qin, Xiangjie, Han Wang, Yuxuan Xia, Wu He, Xuanzhe Xia, and Jianchao Cai. "Three-dimensional modeling of nanoconfined multiphase flow in clay nanopores using FIB-SEM images of shale." Innovation Energy, 2024, 100050. http://dx.doi.org/10.59717/j.xinn-energy.2024.100050.

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<p>Understanding the flow characteristics within shale nanopores is crucial for enhancing hydrocarbon recovery. However, the flow characteristics of wetting and non-wetting fluids on nanopore surfaces differ significantly, limiting the accurate prediction of hydrocarbon accumulation and migration. This work introduces the Euler-Euler volume of fluid method to establish a multiphase flow numerical model in shale nanopores, considering complex pore topology, slip flow, and capillary effects. Based on natural three-dimensional shale nanoporous systems constructed from FIB-SEM images, single

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