KOLÁŘOVÁ, Kristina, Jan ČERNÝ, Rostislav MELICHAR, Petr SCHNABL a Krzysztof GAIDZIK. Reconstruction of ancient volcanic complexes using magnetic signature: A case study from Cambrian andesite lava flow, Bohemian Massif. Journal of Volcanology and Geothermal Research. Elsevier, 2022, roč. 428, August, s. 1-13. ISSN 0377-0273. Dostupné z: https://dx.doi.org/10.1016/j.jvolgeores.2022.107591. |
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@article{1857399, author = {Kolářová, Kristina and Černý, Jan and Melichar, Rostislav and Schnabl, Petr and Gaidzik, Krzysztof}, article_number = {August}, doi = {http://dx.doi.org/10.1016/j.jvolgeores.2022.107591}, keywords = {Andesite; Lava flow; Cambrian; Anisotropy of magnetic susceptibility; Bohemian Massif; Křivoklát-Rokycany Volcanic complex}, language = {eng}, issn = {0377-0273}, journal = {Journal of Volcanology and Geothermal Research}, title = {Reconstruction of ancient volcanic complexes using magnetic signature: A case study from Cambrian andesite lava flow, Bohemian Massif}, url = {https://doi.org/10.1016/j.jvolgeores.2022.107591}, volume = {428}, year = {2022} }
TY - JOUR ID - 1857399 AU - Kolářová, Kristina - Černý, Jan - Melichar, Rostislav - Schnabl, Petr - Gaidzik, Krzysztof PY - 2022 TI - Reconstruction of ancient volcanic complexes using magnetic signature: A case study from Cambrian andesite lava flow, Bohemian Massif JF - Journal of Volcanology and Geothermal Research VL - 428 IS - August SP - 1-13 EP - 1-13 PB - Elsevier SN - 03770273 KW - Andesite KW - Lava flow KW - Cambrian KW - Anisotropy of magnetic susceptibility KW - Bohemian Massif KW - Křivoklát-Rokycany Volcanic complex UR - https://doi.org/10.1016/j.jvolgeores.2022.107591 N2 - Reconstruction of the Upper Cambrian Křivoklát-Rokycany Volcanic Complex was made using anisotropy of magnetic susceptibility (AMS). The correlation of AMS with visible structures at a few sites showed that the most important and reliable information was the direction of magnetic lineation K1 that determines the direction of a lava flow. The analysis of K1 directions together with radially propagating dikes helped to determine the feeding area along the NW rim of the volcanic complex. One andesite feeder and one rhyodacite feeder were recognized with certainty. In addition, K1 directions pointed to a suspicious area with the presence of another andesite feeder in a caldera-like structure. The evaluation of data strongly suggests that magnetic susceptibility in andesite lavas increases with the distance from the feeder and also with the distance towards the upper part of the andesitic lava flow. We suggest that this might be related to the degree of oxidation of the lava flow before solidification as a reaction with oxygen in the atmosphere. Oxygen can react with FeO in the andesite melt, which consequently results in the formation of magnetite. ER -
KOLÁŘOVÁ, Kristina, Jan ČERNÝ, Rostislav MELICHAR, Petr SCHNABL a Krzysztof GAIDZIK. Reconstruction of ancient volcanic complexes using magnetic signature: A case study from Cambrian andesite lava flow, Bohemian Massif. \textit{Journal of Volcanology and Geothermal Research}. Elsevier, 2022, roč.~428, August, s.~1-13. ISSN~0377-0273. Dostupné z: https://dx.doi.org/10.1016/j.jvolgeores.2022.107591.
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