Petrological and Geochemical Characterization of a Granitic Rock from the Velence Mountains, Hungary

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dc.contributor.advisorBenkó, Zsolt
dc.contributor.authorXu, Tianyue
dc.contributor.departmentDE--Természettudományi és Technológiai Kar--Földtudományi Intézet
dc.date.accessioned2026-06-08T08:02:35Z
dc.date.available2026-06-08T08:02:35Z
dc.date.created2026-04-28
dc.description.abstractThe study investigates the geochemical characteristics of a high-K calc-alkaline, weakly peraluminous sample enriched in LILE, Zr, and REE, without a strong negative Eu anomaly. These features suggest formation in a post-collisional extensional environment during the final stages of the Variscan orogeny. The interpretation is supported by regional geological evidence from the Velence Hills, indicating two-phase intrusive activity in the Late Carboniferous to Early Permian period (271–291 Ma). The sample is closely related to Patka-type granite porphyry and reflects later stages of magma evolution associated with extensional fracturing in a cooling batholith. Overall, it records the transition from syn-collisional to post-collisional tectonics and crustal evolution through progressive melting, differentiation, and crustal thinning.
dc.description.courseEarth Sciences
dc.description.degreeBSc/BA
dc.format.extent39
dc.identifier.urihttps://hdl.handle.net/2437/407999
dc.language.isoen
dc.rights.infoHozzáférhető a 2022 decemberi felsőoktatási törvénymódosítás értelmében.
dc.subjectGeochemistry
dc.subjectPetrology
dc.subjectGranitic Rock
dc.subjectValence Mountain
dc.subject.dspaceEarth Sciences
dc.titlePetrological and Geochemical Characterization of a Granitic Rock from the Velence Mountains, Hungary
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