Abstract
Bezymianny volcano eruptions transport numerous xenoliths to the surface. Crustal xenoliths contain unique information about the crust structure and composition of crustal rocks located around the active magmatic system. We describe the chemical and mineral composition of upper crustal xenoliths that pyrometamorphosed (recrystallized and partially melted) in the Bezymianny shallow chamber. We reconstructed protoliths and hydrothermal processes for several rocks, which were previously altered, based on pre-pyrometamorhic relics (primary igneous associations in some xenoliths and rare hydrothermal relics). Moderate-K andesites, basaltic andesites, and basalts of Kamen and Bezymianny volcanoes dominate among the xenoliths. During pyrometamorphism, a microgranoblastic assemblage composed of homogenous pyroxenes, plagioclase, Fe-Ti oxides, and interstitial glass is formed in these xenoliths. Less common xenoliths are presented by high-K basaltic trachyandesite (plateau basalt from the basement of the Klyuchevskaya group of volcanoes). Quartz–carbonate–sulfide mineralization is present in some of them, which formed prior to xenolith entrapment and pyrometamorphism. When xenoliths were entrapped by magma, recrystallization of hydrothermally altered rock produced Fe-wollastonite–hedenbergite association (in some cases with garnet), untypical for Bezymianny. Some of these xenoliths have extremely high copper content (up to 1500 ppm).
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Supplementary 1 available on http://link.springer.com/ presents following data: ESM_1.xlsx—Data on mineral associations in pyrometamorphosed upper crustal xenoliths; ESM_2.xlsx—Representative analyses of pyroxenes from pyrometamorphoes upper crustal xenoliths; ESM_3.xlsx—Representative analyses of plagioclase from pyrometamorphosed upper crustal xenoliths; ESM_4.xlsx—Representative analyses of olivine relict from pyrometamorphosed upper crustal xenoliths; ESM_5.xlsx—Representative analyses of amphibole from pyrometamorphosed upper crustal xenolihs; ESM_6.xlsx—Representative analyses of glass from pyrometamorphosed upper crustal xenoliths; ESM_7.xlsx—Representative analyses of newly formed Fe-Ti oxides from pyrometamorphosed upper crustal xenoliths; ESM_8.xlsx—Representative analyses of newly formed apatite from pyrometamorphosed upper crustal xenoliths; ESM_9.xlsx—Composition of sulfide phases from pyrometamorphosed upper crustal xenoliths; ESM_10.xlsx—Representative analyses of biotite relicts from pyrometamorphosed upper crustal xenoliths; ESM_11.xlsx—Representative analyses of silica phases from pyrometamorphosed upper crustal xenoliths; ESM_12.xlsx—Representative analyses of newly formed garnet from pyrometamorphosed upper crustal xenoliths; ESM_13.xlsx—Representative analyses of newly formed titanite from pyrometamorphosed upper crustal xenoliths. Supplementary 2: ESM_1.pdf—Bulk chemical and modal mineral compositions of studied rocks.
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ACKNOWLEDGMENTS
We are grateful to M.E. Zelenski for field works organization in 2012, to M.D. Shchekleina for help with field works in 2021; S.M. Tolchinsky for helping with sample preparation, and N.N. Koshlyakova for helping with analytical studies. The manuscript was significantly improved by the valuable comments of V.S. Kamentsky and E.V. Sokol.
Funding
The study was supported by the Russian Science Foundation (project no. 22-77-00016).
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Davydova, V.O., Shcherbakov, V.D., Nekrylov, N.A. et al. Sulfide Mineralization in Pyrometamorphosed Upper Crustal Xenoliths, Bezymianny Volcano, Kamchatka. Petrology 31, 358–382 (2023). https://doi.org/10.1134/S0869591123030049
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DOI: https://doi.org/10.1134/S0869591123030049