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the claim
Magnetic surveys can detect archaeological features at varying distances depending on basalt bedrock.
the verdict
INSUFFICIENT LEANING
refutedsupported
the weight of evidence
2 sources for · 0 against

The retrieved evidence mentions magnetic surveying over basalt dikes and basement rocks, but does not provide complete coverage regarding how magnetic detection of archaeological features varies in distance depending on basalt bedrock.

Evidence for · 2
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Abstract We conducted magnetic surveys using an Overhauser magnetometer, a fast-sampling, high-accuracy magnetometer, at two archaeological sites in central Japan to detect magnetic anomalies associated with buried climbing Sue ware kilns in suburban hill areas. Our magnetic survey was conducted in two stages, a preliminary sweeping survey followed by a detailed mapping survey. The mapping survey at both sites revealed magnetic anomalies of the order of 10–100 nT that were clearly distinguishable from the low background signals due to the basement rocks and soils. After the magnetic surveys, a
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The analysis

rails:sufficiency:partial_only:for=0+2p:against=0+0p | v55:multi_partial_one_side:lean=lean_partial:for:one_sided

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Frontiers | Ground Magnetic Surveying and Susceptibility Mapping Across Weathered Basalt Dikes Reveal Soil Creep and Pedoturbation #### Geomagnetism and Paleomagnetism Published inFrontiers in Earth Science 2 impact factor4.3 citescore Part of a Research TopicAdvances in Magnetism of Soils and Sediments86k views15 articles ## BRIEF RESEARCH REPORT article Front. Earth Sci., 15 January 2021 Sec. Geomagnetism and Paleomagnetism Volume 8 - 2020 | https://doi.org/10.3389/feart.2020.592986 # Ground Magnetic Surveying and Susceptibility Mapping Across Weathered Basalt Dikes Reveal Soil Creep and Pedoturbation - TVTilo von Dobeneck * - MMMaximilian Müller - BBBenjamin Bosbach - AKAndreas Klügel Faculty of Geosciences, University of Bremen, Bremen, Germany Article metrics View details ## Abstract Ground magnetic survey profiles across a soil-covered and weathered mafic dike in sedimentary host rock not only permit to delineate the strike, width and burial depth of the intrusive basalt sheet, but also reflect the subsurface deformation of its clayey weathering products. We illustrate this finding and its practical geomorphological applicability by an example from the mid-Germa
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  1. Magnetic survey of archaeological kiln sites with Overhauser magnetometer: A case study of buried Sue ware kilns in Japanpeer-reviewedno side taken
  2. Ground Magnetic Surveying and Susceptibility Mapping ...referenceno side taken
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