Matches in SemOpenAlex for { <https://semopenalex.org/work/W4288045363> ?p ?o ?g. }
Showing items 1 to 95 of
95
with 100 items per page.
- W4288045363 endingPage "106914" @default.
- W4288045363 startingPage "106914" @default.
- W4288045363 abstract "Using the scaling spectral method applied on high resolution aeromagnetic data, we mapped the magnetic basement and estimated the scaling exponents across various lithologies within the Middle Benue Trough of Northcentral Nigeria. We estimated a depth range of 1.8–6.3 km, with an average of 3.7 km to the basement beneath the Cretaceous sediments of the trough. Shallow basement depths of <3 km are mostly found on the trough's northern and southeastern margins. These are uplifted Precambrian Basement Complex regions made up of older granite, gneiss, and migmatite. Deeper basement depths of >4 km predominate in the southwestern, central, and northeastern portions of the study area, trending along the trough's axis. These deep zones are filled with Cretaceous sediments that must have accumulated after the Mesozoic development of the Benue Trough's subsided graben structure. Our study estimated scaling exponent ranging from 0 to 2. There were some correlations with the geology of the area, particularly around the crystalline basement complex in the northern portion. Within the central portion of the Middle Benue Trough, however, the source distributions are less correlated, uneven, and not always consistent with the geology of the area. This could be due to the region's dynamic and unstable tectonics, as numerous magmatic intrusions have been emplaced into the Cretaceous sediments at various depths, potentially influencing the scaling exponent values. • Scaling spectral method was applied on high resolution aeromagnetic data • We estimated a depth range of 1.8–6.3 km to the basement beneath the Cretaceous sediments of the trough and a corresponding scaling exponent ranging from 0 to 2. • There were some correlations with the geology of the area, particularly around the crystalline basement complex in the northern portion. However, the source distributions are less correlated, uneven, and not always consistent with the geology of the area around the central portion which is attributed to intrusions. • This method tends to be more reliable as the degree of correlation of the magnetic sources were taken into account for the first time in most parts of the study area. • As a result, this present work will provide more useful insights into groundwater, mineral, and hydrocarbon explorations in the area." @default.
- W4288045363 created "2022-07-27" @default.
- W4288045363 creator A5033145509 @default.
- W4288045363 creator A5054744668 @default.
- W4288045363 creator A5072276761 @default.
- W4288045363 creator A5078832461 @default.
- W4288045363 creator A5088865880 @default.
- W4288045363 date "2022-10-01" @default.
- W4288045363 modified "2023-09-23" @default.
- W4288045363 title "Application of scaling geology in magnetic basement mapping around the Middle Benue Trough in Northcentral Nigeria" @default.
- W4288045363 cites W1971116545 @default.
- W4288045363 cites W1976060932 @default.
- W4288045363 cites W1987101922 @default.
- W4288045363 cites W1992290075 @default.
- W4288045363 cites W2003372043 @default.
- W4288045363 cites W2004427321 @default.
- W4288045363 cites W2023850930 @default.
- W4288045363 cites W2068991796 @default.
- W4288045363 cites W2087070363 @default.
- W4288045363 cites W2110894291 @default.
- W4288045363 cites W2114851183 @default.
- W4288045363 cites W2133073266 @default.
- W4288045363 cites W2133369047 @default.
- W4288045363 cites W2153408818 @default.
- W4288045363 cites W2155604445 @default.
- W4288045363 cites W2162088010 @default.
- W4288045363 cites W2256578114 @default.
- W4288045363 cites W2520707651 @default.
- W4288045363 cites W2612225252 @default.
- W4288045363 cites W2900499798 @default.
- W4288045363 cites W2900856211 @default.
- W4288045363 cites W2921896241 @default.
- W4288045363 cites W2946768274 @default.
- W4288045363 cites W3008723246 @default.
- W4288045363 cites W3119871059 @default.
- W4288045363 cites W3212476911 @default.
- W4288045363 cites W4211116861 @default.
- W4288045363 doi "https://doi.org/10.1016/j.pepi.2022.106914" @default.
- W4288045363 hasPublicationYear "2022" @default.
- W4288045363 type Work @default.
- W4288045363 citedByCount "1" @default.
- W4288045363 countsByYear W42880453632023 @default.
- W4288045363 crossrefType "journal-article" @default.
- W4288045363 hasAuthorship W4288045363A5033145509 @default.
- W4288045363 hasAuthorship W4288045363A5054744668 @default.
- W4288045363 hasAuthorship W4288045363A5072276761 @default.
- W4288045363 hasAuthorship W4288045363A5078832461 @default.
- W4288045363 hasAuthorship W4288045363A5088865880 @default.
- W4288045363 hasConcept C114793014 @default.
- W4288045363 hasConcept C127313418 @default.
- W4288045363 hasConcept C139719470 @default.
- W4288045363 hasConcept C151730666 @default.
- W4288045363 hasConcept C162324750 @default.
- W4288045363 hasConcept C165205528 @default.
- W4288045363 hasConcept C166957645 @default.
- W4288045363 hasConcept C205649164 @default.
- W4288045363 hasConcept C2524010 @default.
- W4288045363 hasConcept C2781297371 @default.
- W4288045363 hasConcept C32239851 @default.
- W4288045363 hasConcept C33923547 @default.
- W4288045363 hasConcept C8058405 @default.
- W4288045363 hasConcept C99844830 @default.
- W4288045363 hasConceptScore W4288045363C114793014 @default.
- W4288045363 hasConceptScore W4288045363C127313418 @default.
- W4288045363 hasConceptScore W4288045363C139719470 @default.
- W4288045363 hasConceptScore W4288045363C151730666 @default.
- W4288045363 hasConceptScore W4288045363C162324750 @default.
- W4288045363 hasConceptScore W4288045363C165205528 @default.
- W4288045363 hasConceptScore W4288045363C166957645 @default.
- W4288045363 hasConceptScore W4288045363C205649164 @default.
- W4288045363 hasConceptScore W4288045363C2524010 @default.
- W4288045363 hasConceptScore W4288045363C2781297371 @default.
- W4288045363 hasConceptScore W4288045363C32239851 @default.
- W4288045363 hasConceptScore W4288045363C33923547 @default.
- W4288045363 hasConceptScore W4288045363C8058405 @default.
- W4288045363 hasConceptScore W4288045363C99844830 @default.
- W4288045363 hasLocation W42880453631 @default.
- W4288045363 hasOpenAccess W4288045363 @default.
- W4288045363 hasPrimaryLocation W42880453631 @default.
- W4288045363 hasRelatedWork W134098704 @default.
- W4288045363 hasRelatedWork W1992202538 @default.
- W4288045363 hasRelatedWork W2018160905 @default.
- W4288045363 hasRelatedWork W2091305899 @default.
- W4288045363 hasRelatedWork W2097394790 @default.
- W4288045363 hasRelatedWork W2099516475 @default.
- W4288045363 hasRelatedWork W2900481724 @default.
- W4288045363 hasRelatedWork W2995812845 @default.
- W4288045363 hasRelatedWork W3216216372 @default.
- W4288045363 hasRelatedWork W321724292 @default.
- W4288045363 hasVolume "331" @default.
- W4288045363 isParatext "false" @default.
- W4288045363 isRetracted "false" @default.
- W4288045363 workType "article" @default.