Mineralogical changes during thermal demagnetization of natural continental sandstones
| Autor: | R. C. Mercader, Rubén Somoza, Claudia Beatriz Prezzi |
|---|---|
| Rok vydání: | 2005 |
| Předmět: |
cement
Geochemistry Hematite Mineralogy Maghemite engineering.material Natural (archaeology) Transformation Magnetite chemistry.chemical_compound Siderite Geochemistry and Petrology Mössbauer spectroscopy Cement Geofísica Geophysics chemistry visual_art visual_art.visual_art_medium engineering Structural geology Geology |
| Zdroj: | SEDICI (UNLP) Universidad Nacional de La Plata instacron:UNLP |
| ISSN: | 1573-1626 0039-3169 |
| DOI: | 10.1007/s11200-005-0006-4 |
| Popis: | We study the mineralogical changes suffered by specimens of natural miocene red and green continental sandstones (from Pozuelos Formation and Tiomayo Formation) cropping out in the Argentine Puna that increase their bulk magnetic susceptibility and change color when thermally treated. We hypothesize that on heating siderite, which is present in small quantities as cement in the studied sandstones, would oxidize and decompose into maghemite and/or magnetite. Subsequent heating to higher temperatures sometimes would bring about the conversion of maghemite and/or magnetite to hematite. Mossbauer spectroscopy proved to be a very valuable tool for the determination of the presence of siderite in small amounts in the studied samples. The present results show that further work is needed in order to fully understand the mineralogical changes suffered by continental sandstones during heating. The characterization of such changes occurred during laboratory routines is relevant, since they can help to better understand natural processes. Instituto de Física La Plata |
| Databáze: | OpenAIRE |
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