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| Titel |
The correlation of attenuated total reflectance infrared (ATR-FTIR) spectroscopic data with X-ray diffraction (XRD) parameters and its potential use for mineral identification and quantification in drilling cores: examples from the Pannonian Basin, Hungar |
| VerfasserIn |
Beatrix Udvardi, István Kovács, István Viczián, Mária Hámor-Vidó, Judith Mihály, Csaba Németh |
| Konferenz |
EGU General Assembly 2013
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 15 (2013) |
| Datensatznummer |
250081629
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| Zusammenfassung |
| Four thick sediment sequences in the following boreholes, Vízvár-I (0,0-2965,0 m) in the
Dráva Basin, Som-I (999,5-1150,6 m) in southern Transdanubia, and two other boreholes,
Doboz-I (3490-4434 m) and Doboz-III (2190-3400 m) in the Békés Basin, Hungary, were
investigated in detail. Each drillings cut across Neogene sequences and contain
shales, carbonates and clay rocks (Tanács & Viczián, 1995). The selection of these
cores is due to the various amounts of smectite, illite and kaolinite minerals that are
well manifested during comparison of infrared spectroscopic and former XRD
dataset.
During preparation, powdered core samples were settled ( |
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