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- W2592640266 abstract "A combined thermal and magnetic evaluation on experimentally knapped clasts of different lithologies (chert, quartzite, limestone, sandstone and obsidian) heated under controlled field and temperature conditions were carried out. The main aim of this study is to estimate the feasibility of use of these raw materials, which are commonly found in prehistoric archaeological sites, for archaeomagnetic purposes. Rock magnetic analysis included measurements of low-field magnetic susceptibility, isothermal remanent magnetisation (IRM) acquisition curves, hysteresis loops and thermomagnetic curves of lithic clasts both before and after experimental heating. All lithologies, except the obsidian, recorded an increase of up two orders of magnitude in their magnetic concentration-dependent parameters revealing the formation of new ferrimagnetic minerals. Obsidian and sandstone are the most reliable magnetic carriers, followed by limestone, chert and quartzite. Magnetic susceptibility values show significant differences among lithologies. Isothermal remanent magnetisation proved also to be highly discriminatory as well as the room temperature hysteresis parameters. The main macroscopic alterations resulted in colour changes, rubefactions, potlids in cherts and the massive formation of internal fissures in obsidian specimens. The multispecimen absolute geomagnetic intensity technique was applied on selected samples yielding satisfactory results for heated obsidian and sandstone samples. The archaeological applicability of the results is discussed as well as their geomagnetic significance." @default.
- W2592640266 created "2017-03-16" @default.
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- W2592640266 date "2013-01-01" @default.
- W2592640266 modified "2023-09-23" @default.
- W2592640266 title "ROCK-MAGNETIC PROPERTIES AND ABSOLUTE PALEOINTENSITY DETERMINATION ON LITHIC CLASTS BURNED UNDER CONTROLLED TEMPERATURE AND FIELD CONDITIONS: ARCHAEOLOGICAL AND GEOMAGNETIC IMPLICATIONS" @default.
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