2026
Correlative imaging of large-scale geological samples using LIBS and SEM-EDX automated mineralogy
BUDAY, Jakub; Jakub VÝRAVSKÝ; Jan CEMPÍREK; David PROCHAZKA; Pavel PORIZKA et al.Základní údaje
Originální název
Correlative imaging of large-scale geological samples using LIBS and SEM-EDX automated mineralogy
Autoři
BUDAY, Jakub; Jakub VÝRAVSKÝ; Jan CEMPÍREK; David PROCHAZKA; Pavel PORIZKA a Jozef KAISER
Vydání
SPECTROCHIMICA ACTA PART B-ATOMIC SPECTROSCOPY, OXFORD, PERGAMON-ELSEVIER SCIENCE LTD, 2026, 0584-8547
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10504 Mineralogy
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 3.800 v roce 2024
Označené pro přenos do RIV
Ano
Organizační jednotka
Přírodovědecká fakulta
UT WoS
EID Scopus
Klíčová slova anglicky
Multi-elemental imaging; Clustering; Geology; Automated mineralogy; lithium; Pegmatites
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 11. 3. 2026 16:13, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
Elemental mapping of light (Li, Be, B, F) and trace elements in large-area geological samples represents an analytical challenge. Increased interest in Li and rare-element deposits results in the need for reliable mapping of light and trace elements. One of the possible solutions is laser-induced breakdown spectroscopy (LIBS) combined with sophisticated data processing. We studied four large-area (ca. 8 & Cross;8 cm) samples from two rare-element Berich granitic pegmatites with moderate contents of Li + Be (Mars & iacute;kov, Czech Republic) and high contents of Li + Be+B (Rau property, Yukon, Canada). Cross-sections from the host rock to the geochemically evolved center of the pegmatite were used for direct multi-element mapping, assisted semi-automated machine-learning-based mineral identification, and tracing of magmatic, metasomatic and hydrothermal processes. From the obtained LIBS data, elemental images of individual elements of interest were produced (incl. Li and Be), and unsupervised clustering to the spectra was applied. This led to cluster images manifesting the distribution of individual matrices (i.e., minerals). The outputs of clustering were visually and statistically compared to a phase map produced by a state-of-the-art SEM-EDS-based Automated mineralogy solution (TIMA) and the results show good agreement. The study demonstrates a very good applicability of LIBS for the detection and mapping of major (Si, Al, Fe, Mg, Mn, Ca, Na), light elements (Li, Be, B, F), and trace elements (Ge, Ga, Cu, Ti, Sr, Ba) in pegmatites, discerning their specific geochemical signatures corresponding to magmatic, metasomatic, and hydrothermal stage of their evolution. The EDS-based automated mineralogy offers a higher spatial resolution in general. Still, it cannot map light elements (H, Li, Be, B) and has between one to three orders of magnitude worse detection limit for many other elements (e.g. Ga...).
Návaznosti
| TH79020002, projekt VaV |
|