Abstract
The primary goals of this research are the geochemistry and identification of granite rocks. The granitic rocks are part of the Syrostan massive, which is located in southern Ural. Understanding the magma process and probable mineralization deposition can be gained by classifying granite and determining geochemical characteristics. X-ray spectral fluorescence analysis was used to collect samples from outcrops for geochemical analysis. The results indicate that the rocks belong to the high-k calc alkaline to calc alkaline series. The granites are metaluminous to slightly peraluminous and are classified as I-type granites, with A/CNK values ranging from 0.73 to 1.01. The majority of the rock samples are trondhjemite to slightly tonalite in composition. The most observable samples in the normative Na2OkO-CaO scheme have defined a continuous range, ranging from tonalite/trondhjemite to granodiorite. The implications of the findings provide valuable information about the petrogenesis of the rocks and their composition.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: News of the Tula state university. Sciences of Earth
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
