Articles | Volume 34, issue 1
https://doi.org/10.5194/ejm-34-7-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/ejm-34-7-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
40Ar/39Ar dating of a hydrothermal pegmatitic buddingtonite–muscovite assemblage from Volyn, Ukraine
Gerhard Franz
CORRESPONDING AUTHOR
Institut für Angewandte Geowissenschaften, Technische
Universität Berlin, Berlin, 10587, Germany
Masafumi Sudo
Institut für Geowissenschaften, Universität Potsdam, Potsdam, 14476, Germany
Vladimir Khomenko
Semenenko Institute of Geochemistry, Mineralogy, and Ore Formation,
National Academy of Sciences of Ukraine, pr. Palladina 34, Kiev, 03680
Ukraine
Related authors
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chournousenko, and Ulrich Struck
Biogeosciences, 21, 4119–4131, https://doi.org/10.5194/bg-21-4119-2024, https://doi.org/10.5194/bg-21-4119-2024, 2024
Short summary
Short summary
The Volyn biota (Ukraine), previously assumed to be an extreme case of natural abiotic synthesis of organic matter, is more likely a diverse assemblage of fossils from the deep biosphere. Although contamination by modern organisms cannot completely be ruled out, it is unlikely, considering all aspects, i.e., their mode of occurrence in the deep biosphere, their fossilization and mature state of organic matter, their isotope signature, and their large morphological diversity.
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chournousenko, Ulrich Struck, Ulrich Gernert, and Jörg Nissen
Biogeosciences, 20, 1901–1924, https://doi.org/10.5194/bg-20-1901-2023, https://doi.org/10.5194/bg-20-1901-2023, 2023
Short summary
Short summary
This research describes the occurrence of Precambrian fossils, with exceptionally well preserved morphology in 3D. These microfossils reach a size of millimeters (possibly up to centimeters) and thus indicate the presence of multicellular eukaryotes. Many of them are filamentous, but other types were also found. These fossils lived in a depth of several hundred meters and thus provide good evidence of a continental the deep biosphere, from a time generally considered as the
boring billion.
Gerhard Franz, Peter Lyckberg, Vladimir Khomenko, Vsevolod Chournousenko, Hans-Martin Schulz, Nicolaj Mahlstedt, Richard Wirth, Johannes Glodny, Ulrich Gernert, and Jörg Nissen
Biogeosciences, 19, 1795–1811, https://doi.org/10.5194/bg-19-1795-2022, https://doi.org/10.5194/bg-19-1795-2022, 2022
Short summary
Short summary
In pegmatites from Ukraine Precambrian fossils between 1.5 Ga and 1.76 Ga were preserved in cavities connected to the surface in a geyser system. The fossilization process is silicification of the outermost rim of the fossils, stabilizing the remaining part of the organisms. The variety of organisms points to an ecosystem of several microorganisms which was active in the continental environment, and igneous rocks such as the pegmatites seem to be an ideal habitat for the deep biosphere.
Leonid Shumlyanskyy, Gerhard Franz, Sarah Glynn, Oleksandr Mytrokhyn, Dmytro Voznyak, and Olena Bilan
Eur. J. Mineral., 33, 703–716, https://doi.org/10.5194/ejm-33-703-2021, https://doi.org/10.5194/ejm-33-703-2021, 2021
Short summary
Short summary
In the paper we discuss the origin of large chamber pegmatite bodies which contain giant gem-quality crystals of black quartz (morion), beryl, and topaz. We conclude that these pegmatites develop under the influence of later intrusions of mafic rocks that cause reheating of the partly crystallized granite massifs and that they supply a large amount of fluids that facilitate the
inflationof pegmatite chambers and crystallization of giant crystals of various minerals.
Gerhard Franz, Martin Kutzschbach, Eleanor J. Berryman, Anette Meixner, Anselm Loges, and Dina Schultze
Eur. J. Mineral., 33, 401–423, https://doi.org/10.5194/ejm-33-401-2021, https://doi.org/10.5194/ejm-33-401-2021, 2021
Short summary
Short summary
Metamorphic rocks contain information about their original rocks and thus provide insight into the earlier stages of a region of interest. Here, we used the whole-rock chemical composition and stable boron isotopes of a suite of rocks from the Alps (Italy–Austria), which were deposited in a restricted intramontane basin before the Alpine orogeny. It is possible to reconstruct the depositional conditions for these sediments, which are now common metamorphic rocks such as schists and gneisses.
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chournousenko, and Ulrich Struck
Biogeosciences, 21, 4119–4131, https://doi.org/10.5194/bg-21-4119-2024, https://doi.org/10.5194/bg-21-4119-2024, 2024
Short summary
Short summary
The Volyn biota (Ukraine), previously assumed to be an extreme case of natural abiotic synthesis of organic matter, is more likely a diverse assemblage of fossils from the deep biosphere. Although contamination by modern organisms cannot completely be ruled out, it is unlikely, considering all aspects, i.e., their mode of occurrence in the deep biosphere, their fossilization and mature state of organic matter, their isotope signature, and their large morphological diversity.
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chournousenko, Ulrich Struck, Ulrich Gernert, and Jörg Nissen
Biogeosciences, 20, 1901–1924, https://doi.org/10.5194/bg-20-1901-2023, https://doi.org/10.5194/bg-20-1901-2023, 2023
Short summary
Short summary
This research describes the occurrence of Precambrian fossils, with exceptionally well preserved morphology in 3D. These microfossils reach a size of millimeters (possibly up to centimeters) and thus indicate the presence of multicellular eukaryotes. Many of them are filamentous, but other types were also found. These fossils lived in a depth of several hundred meters and thus provide good evidence of a continental the deep biosphere, from a time generally considered as the
boring billion.
Gerhard Franz, Peter Lyckberg, Vladimir Khomenko, Vsevolod Chournousenko, Hans-Martin Schulz, Nicolaj Mahlstedt, Richard Wirth, Johannes Glodny, Ulrich Gernert, and Jörg Nissen
Biogeosciences, 19, 1795–1811, https://doi.org/10.5194/bg-19-1795-2022, https://doi.org/10.5194/bg-19-1795-2022, 2022
Short summary
Short summary
In pegmatites from Ukraine Precambrian fossils between 1.5 Ga and 1.76 Ga were preserved in cavities connected to the surface in a geyser system. The fossilization process is silicification of the outermost rim of the fossils, stabilizing the remaining part of the organisms. The variety of organisms points to an ecosystem of several microorganisms which was active in the continental environment, and igneous rocks such as the pegmatites seem to be an ideal habitat for the deep biosphere.
Leonid Shumlyanskyy, Gerhard Franz, Sarah Glynn, Oleksandr Mytrokhyn, Dmytro Voznyak, and Olena Bilan
Eur. J. Mineral., 33, 703–716, https://doi.org/10.5194/ejm-33-703-2021, https://doi.org/10.5194/ejm-33-703-2021, 2021
Short summary
Short summary
In the paper we discuss the origin of large chamber pegmatite bodies which contain giant gem-quality crystals of black quartz (morion), beryl, and topaz. We conclude that these pegmatites develop under the influence of later intrusions of mafic rocks that cause reheating of the partly crystallized granite massifs and that they supply a large amount of fluids that facilitate the
inflationof pegmatite chambers and crystallization of giant crystals of various minerals.
Gerhard Franz, Martin Kutzschbach, Eleanor J. Berryman, Anette Meixner, Anselm Loges, and Dina Schultze
Eur. J. Mineral., 33, 401–423, https://doi.org/10.5194/ejm-33-401-2021, https://doi.org/10.5194/ejm-33-401-2021, 2021
Short summary
Short summary
Metamorphic rocks contain information about their original rocks and thus provide insight into the earlier stages of a region of interest. Here, we used the whole-rock chemical composition and stable boron isotopes of a suite of rocks from the Alps (Italy–Austria), which were deposited in a restricted intramontane basin before the Alpine orogeny. It is possible to reconstruct the depositional conditions for these sediments, which are now common metamorphic rocks such as schists and gneisses.
Related subject area
Igneous petrology
Magmatic to solid-state evolution of a shallow emplaced agpaitic tinguaite (the Suc de Sara dyke, Velay volcanic province, France): implications for peralkaline melt segregation and extraction in ascending magmas
Granite magmatism and mantle filiation
Inclusions in magmatic zircon from Slavonian mountains (eastern Croatia): anatase, kumdykolite and kokchetavite and implications for the magmatic evolution
Confocal μ-XANES as a tool to analyze Fe oxidation state in heterogeneous samples: the case of melt inclusions in olivine from the Hekla volcano
Constraining the volatile evolution of mafic melts at Mt. Somma–Vesuvius, Italy, based on the composition of reheated melt inclusions and their olivine hosts
Contrasting appinites, vaugnerites and related granitoids from the NW Iberian Massif: insight into mantle and crustal sources
Reactive interaction between migmatite-related melt and mafic rocks: clues from the Variscan lower crust of Palmi (southwestern Calabria, Italy)
ICDP Oman Drilling Project: varitextured gabbros from the dike–gabbro transition within drill core GT3A
A snapshot of the transition from monogenetic volcanoes to composite volcanoes: case study on the Wulanhada Volcanic Field (northern China)
Geochronology of granites of the western Korosten AMCG complex (Ukrainian Shield): implications for the emplacement history and origin of miarolitic pegmatites
A new clinopyroxene thermobarometer for mafic to intermediate magmatic systems
Quantification of major and trace elements in fluid inclusions and gas bubbles by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) with no internal standard: a new method
New evidence for upper Permian crustal growth below Eifel, Germany, from mafic granulite xenoliths
Contaminating melt flow in magmatic peridotites from the lower continental crust (Rocca d'Argimonia sequence, Ivrea–Verbano Zone)
Thomas Pereira, Laurent Arbaret, Juan Andújar, Mickaël Laumonier, Monica Spagnoli, Charles Gumiaux, Gautier Laurent, Aneta Slodczyk, and Ida Di Carlo
Eur. J. Mineral., 36, 491–524, https://doi.org/10.5194/ejm-36-491-2024, https://doi.org/10.5194/ejm-36-491-2024, 2024
Short summary
Short summary
This work presents the results on deformation-enhanced melt segregation and extraction in a phonolitic magma emplaced at shallow depth in the Velay volcanic province (France). We provide evidence of the segregation and subsequent extraction of the residual melt during magma ascent and final emplacement. We highlight that melt segregation started by compaction as a loose packing of microlites emerged and continued with melt filling of a shear band network.
Michel Pichavant, Arnaud Villaros, Julie A.-S. Michaud, and Bruno Scaillet
Eur. J. Mineral., 36, 225–246, https://doi.org/10.5194/ejm-36-225-2024, https://doi.org/10.5194/ejm-36-225-2024, 2024
Short summary
Short summary
Models for the generation of silicic magmas are divided into two groups: intra-crustal melting and basaltic origin. Peraluminous felsic leucogranites are considered as the only granite examples showing no mantle input. This interpretation is re-evaluated, and we show that leucogranites, as most other crustal granite types, can have a mantle filiation. This stresses the critical importance of the mantle for granite generation and opens the way for unification of silicic magma generation models.
Petra Schneider and Dražen Balen
Eur. J. Mineral., 36, 209–223, https://doi.org/10.5194/ejm-36-209-2024, https://doi.org/10.5194/ejm-36-209-2024, 2024
Short summary
Short summary
The acid igneous rocks of eastern Croatia related to the Late Cretaceous closure of the Neotethys Ocean contain zircon as a main accessory mineral. Among others, zircon has inclusions of anatase, hematite and melt (nanogranitoids) with kokchetavite and kumdykolite. The first finding here of kokchetavite and kumdykolite in a magmatic nanogranitoid proves that these are not exclusively ultra-high pressure phases. The detected inclusions indicate rapid uplift and cooling of the oxidised magma.
Roman Botcharnikov, Max Wilke, Jan Garrevoet, Maxim Portnyagin, Kevin Klimm, Stephan Buhre, Stepan Krasheninnikov, Renat Almeev, Severine Moune, and Gerald Falkenberg
Eur. J. Mineral., 36, 195–208, https://doi.org/10.5194/ejm-36-195-2024, https://doi.org/10.5194/ejm-36-195-2024, 2024
Short summary
Short summary
The new spectroscopic method, based on the syncrotron radiation, allows for determination of Fe oxidation state in tiny objects or in heterogeneous samples. This technique is expected to be an important tool in geosciences unraveling redox conditions in rocks and magmas as well as in material sciences providing constraints on material properties.
Rosario Esposito, Daniele Redi, Leonid V. Danyushevsky, Andrey Gurenko, Benedetto De Vivo, Craig E. Manning, Robert J. Bodnar, Matthew Steele-MacInnis, and Maria-Luce Frezzotti
Eur. J. Mineral., 35, 921–948, https://doi.org/10.5194/ejm-35-921-2023, https://doi.org/10.5194/ejm-35-921-2023, 2023
Short summary
Short summary
Despite many articles published about eruptions at Mt. Somma–Vesuvius (SV), the volatile contents of magmas associated with mafic (quasi-primitive) melts were not directly analyzed for many eruptions based on melt inclusions (MIs). We suggest that several high-Fo olivines formed at depths greater than those of the carbonate platform based on MI chemical composition. We also estimated that 347 to 686 t d-1 of magmatic CO2 exsolved from SV magmas during the last 3 centuries of volcanic activity.
Gumer Galán, Gloria Gallastegui, Andrés Cuesta, Guillermo Corretgé, Ofelia Suárez, and Luis González-Menéndez
Eur. J. Mineral., 35, 845–871, https://doi.org/10.5194/ejm-35-845-2023, https://doi.org/10.5194/ejm-35-845-2023, 2023
Short summary
Short summary
Two examples of granites in the Variscan Iberian Massif were studied because they are associated with mafic rocks (appinites and vaugnerites), which raise the question of the role of mantle magma in the formation of granitic rocks. We conclude that appinites and vaugnerites derived from melting of different mantle sources, both previously modified by interaction with crustal materials. Subsequent differentiation of appinites and vaugnerites was influenced by contamination with coeval granites.
Maria Rosaria Renna
Eur. J. Mineral., 35, 1–24, https://doi.org/10.5194/ejm-35-1-2023, https://doi.org/10.5194/ejm-35-1-2023, 2023
Short summary
Short summary
Distribution of major and trace elements during anatexis at the source area was investigated in a portion of Variscan mid–lower crust exposed at Palmi (Calabria, Italy). Reactive migration of migmatitic melt imparted a mineralogical and chemical signature in mafic rocks associated with migmatites and promoted the crystallization of amphibole by a coupled dissolution–precipitation process. Amphibole and accessory allanite control the distribution of incompatible elements from the anatectic zone.
Artur Engelhardt, Jürgen Koepke, Chao Zhang, Dieter Garbe-Schönberg, and Ana Patrícia Jesus
Eur. J. Mineral., 34, 603–626, https://doi.org/10.5194/ejm-34-603-2022, https://doi.org/10.5194/ejm-34-603-2022, 2022
Short summary
Short summary
We present a detailed petrographic, microanalytical and bulk-chemical investigation of 36 mafic rocks from drill hole GT3A from the dike–gabbro transition zone. These varitextured gabbros are regarded as the frozen fillings of axial melt lenses. The oxide gabbros could be regarded as frozen melts, whereas the majority of the rocks, comprising olivine-bearing gabbros and gabbros, show a distinct cumulate character. Also, we present a formation scenario for the varitextured gabbros.
Diao Luo, Marc K. Reichow, Tong Hou, M. Santosh, Zhaochong Zhang, Meng Wang, Jingyi Qin, Daoming Yang, Ronghao Pan, Xudong Wang, François Holtz, and Roman Botcharnikov
Eur. J. Mineral., 34, 469–491, https://doi.org/10.5194/ejm-34-469-2022, https://doi.org/10.5194/ejm-34-469-2022, 2022
Short summary
Short summary
Volcanoes on Earth are divided into monogenetic and composite volcanoes based on edifice shape. Currently the evolution from monogenetic to composite volcanoes is poorly understood. There are two distinct magma chambers, with a deeper region at the Moho and a shallow mid-crustal zone in the Wulanhada Volcanic Field. The crustal magma chamber represents a snapshot of transition from monogenetic to composite volcanoes, which experience more complex magma processes than magma stored in the Moho.
Leonid Shumlyanskyy, Gerhard Franz, Sarah Glynn, Oleksandr Mytrokhyn, Dmytro Voznyak, and Olena Bilan
Eur. J. Mineral., 33, 703–716, https://doi.org/10.5194/ejm-33-703-2021, https://doi.org/10.5194/ejm-33-703-2021, 2021
Short summary
Short summary
In the paper we discuss the origin of large chamber pegmatite bodies which contain giant gem-quality crystals of black quartz (morion), beryl, and topaz. We conclude that these pegmatites develop under the influence of later intrusions of mafic rocks that cause reheating of the partly crystallized granite massifs and that they supply a large amount of fluids that facilitate the
inflationof pegmatite chambers and crystallization of giant crystals of various minerals.
Xudong Wang, Tong Hou, Meng Wang, Chao Zhang, Zhaochong Zhang, Ronghao Pan, Felix Marxer, and Hongluo Zhang
Eur. J. Mineral., 33, 621–637, https://doi.org/10.5194/ejm-33-621-2021, https://doi.org/10.5194/ejm-33-621-2021, 2021
Short summary
Short summary
In this paper we calibrate a new empirical clinopyroxene-only thermobarometer based on new models. The new models show satisfying performance in both calibration and the test dataset compared with previous thermobarometers. Our new thermobarometer has been tested on natural clinopyroxenes in the Icelandic eruptions. The results show good agreement with experiments. Hence, it can be widely used to elucidate magma storage conditions.
Anastassia Y. Borisova, Stefano Salvi, German Velasquez, Guillaume Estrade, Aurelia Colin, and Sophie Gouy
Eur. J. Mineral., 33, 305–314, https://doi.org/10.5194/ejm-33-305-2021, https://doi.org/10.5194/ejm-33-305-2021, 2021
Short summary
Short summary
We developed a new method for quantifying elemental concentrations in natural and synthetic fluid inclusions and gas bubbles using a laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) method with no internal standard. The method may be applied to estimate trace (metal and metalloid) elemental concentrations in hydrous carbonic (C–O–H) fluid inclusions and bubbles with uncertainty below 25 %.
Cliff S. J. Shaw
Eur. J. Mineral., 33, 233–247, https://doi.org/10.5194/ejm-33-233-2021, https://doi.org/10.5194/ejm-33-233-2021, 2021
Short summary
Short summary
Volcanic activity in the West Eifel region of Germany over the past million years has brought many samples of the Earth's mantle and crust to the surface. The samples from this study are pieces of the deep crust that formed between 264 and 253 million years ago at a depth of ~ 30 km. Samples like these reveal how the Earth's crust has grown and been modified over time.
Marta Antonicelli, Riccardo Tribuzio, Tong Liu, and Fu-Yuan Wu
Eur. J. Mineral., 32, 587–612, https://doi.org/10.5194/ejm-32-587-2020, https://doi.org/10.5194/ejm-32-587-2020, 2020
Short summary
Short summary
We present a petrological–geochemical investigation of peridotites of magmatic origin from the Ivrea–Verbano Zone (Italian Alps), a large-scale section of lower continental crust. The main purpose is to provide new insights into the processes governing the evolution of primitive mantle magmas. We propose that studied peridotites were formed by reaction of a melt-poor olivine-rich crystal mush, or a pre-existing peridotite, with upward-migrating melts possessing a substantial crustal component.
Cited articles
Barker, D. S.: Ammonium in alkali feldspars, Amer. Mineral., 49, 851–858, 1964.
Dai, S., Xie, P., French, D., Ward, C. R., Graham, I. T., Yan, X., and Guo,
W.: The occurrence of buddingtonite in super-high-organic-sulphur coals from
the Yishan Coalfield, Guangxi, southern China, Intern. J. Coal Geol., 195,
347–361, 2018.
Day, R. and Jones, B.: Variations in water content in opal-A and opal-C-T
from geyser discharge aprons, J. Sed. Res., 78, 301–315, 2008.
Di Vicenzo, G., Ghiribelli, B., Giorgetti, G., and Palmeri, R.: Evidence of
a close link between petrology and isotope records: constraints from SEM,
EMP, TEM and in situ 40Ar-39Ar laser analyses on multiple
generations of white micas (Lanterman Range, Antarctica), Earth. Planet.
Sci. Let., 192, 389–405, 2001.
Erd, R. C., White, D. E., Fahey, J. J., and Lee, D. E.: Buddingtonite, an
ammonium feldspar with zeolitic water, Amer. Mineral., 49, 831–850, 1964.
Foland, K. A.: Argon Diffusion in Feldspars, in: Feldspars
and their Reactions, edited by: Parsons, I., NATO ASI Series (Series C: Mathematical and Physical Sciences), vol. 421, Springer, Dordrecht, https://doi.org/10.1007/978-94-011-1106-5_11, 1994.
Franz, G., Khomenko, V., Vishnyevskyy, A., Wirth, R., Struck, U., Nissen,
J., Gernert, U., and Rocholl, A.: Biologically mediated crystallization of
buddingtonite in the Paleoproterozoic: Organic-igneous interactions from the
Volyn pegmatite, Ukraine, Amer. Mineral., 102, 2119–2135, 2017.
Gigashvili, G. M. and Kalyuzhnyi, V. A.: Black opals from Volynian
pegmatites, containing organic matter, Doklady Akademii Nauk SSSR, 186,
1154–1157, 1969 (in Russian).
Gorlenko, V. M., Zhmur, S. I., Duda, V. I., Suzina, N. E., Osipov, G. A.,
and Dimitriev, V. V.: Fine structure of fossilized bacteria in Volyn kerite,
Orig. Life Evol. Biosph., 30, 567–577, 2000.
Gorokhov, I. M., Clauer, N., Varshavskaya, E. S., Kutyavin, E. P., and
Drannik, A. S.: Rb-Sr ages of Precambrian sediments from the Ovruch mountain
range, northwestern Ukraine (U.S.S.R.), Precam. Res., 16, 55–65, 1981.
Graetsch, H.: Structural characteristics of opaline and microcrystalline
silica minerals, Reviews Min. Geochem., 29, 209–232, 1994.
Gulbrandsen, R. A.: Buddingtonite, ammonium feldspar, in the Phosphoria
Formation, southeastern Idaho, J. Res. US Geol. Surv., 2.6, 693–697, 1974.
Halama, R., Konrad-Schmolke, M., Sudo, M., Marschall, H., and Wiedenbeck,
M.: Effects of fluid-rock interaction on 40Ar/39Ar geochronology in high-pressure rocks (Sesia-Lanzo Zone, Western Alps), Geochim. Cosmochim. Acta, 126, 475–494, 2014.
Harlov, D. E., Andrut, M., and Pöter, B.: Characterisation of
buddingtonite (NH4)[AlSi3O8], Phys. Chem. Min., 28, 188–198,
2001.
Ishizuka, O.: Vertical and horizontal variations of the fast neutron flux in
a single irradiation capsule and their significance in the laser-heating
40Ar/39Ar analysis: Case study for the hydraulic rabbit facility of the JMTR reactor, Japan, Geochem. J., 32, 243–252, 1998.
Krooss, B. M., Friberg, L., Gensterblum, Y., Hollenstein, J., Prinz, D., and
Littke R.: Investigation of the pyrolytic liberation of molecular nitrogen
from Palaeozoic sedimentary rocks, Inter. J. Earth Sci., 94, 1023–1038,
2005.
Lanphere, M. A. and Baadsgaard, H.: Precise K-Ar, 40Ar/39Ar, Rb-Sr and U Pb mineral ages from the 27.5 Ma Fish Canyon Tuff reference standard, Chem. Geol., 175, 653–671, 2001.
Laricheva, O. O., Akhmanova, M. V., and Byvhkov, A. M.: Low-temperature
hydrothermal synthesis of buddingtonite, Geochem. Inter., 30, 126–132,
1993.
Loughnan, F. C., Roberts, F. I., and Lindner, A. W.: Buddingtonite
(NH4-feldspar) in the Condor oilshale deposit, Queensland, Australia,
Mineral. Mag., 47, 327–334, 1983.
Lyckberg, P., Chernousenko, V., and Wilson, W. E.: Famous mineral
localities: Volodarsk-Volynski, Zhitomir Oblast, Ukraine, Mineral. Rec., 40, 473–506, 2009.
Lyckberg, P., Chournousenko, V., and Chournousenko, O.: Giant heliodor and
topaz pockets of the Volodarsk chamber pegmatites, Korosten pluton, Ukraine,
36th Intern. Gemmol. Conf., 27–31 August 2019, Nantes, France, 78–83, available at: https://www.igc-gemmology.org/igc-2019 (last access: 11 January 2022), 2019.
Mark D. F., Kelley, S. P., Lee, M. R., Parnell, J., Sherlock, S. C., and
Brown, D. J.: Ar–Ar dating of authigenic K-feldspar: Quantitative modelling of radiogenic argon-loss through subgrain boundary networks, Geochim. Cosmochim. Acta, 72, 2695–2710, 2008.
Muñoz, J. L. and Eugster, H. P.: Experimental control of fluorine
reactions in hydrothermal systems, Amer. Mineral., 54, 943–959, 1969.
Naumenko-Dèzes, M. O., Villa, I. M., Rolland, Y., Gallet, S., and
Lanari, P.: Subgrain 40Ar/39Ar dating of museum-quality micas reveals intragrain heterogeneity, Chem. Geol., 573, 120215, https://doi.org/10.1016/j.chemgeo.2021.120215, 2021.
Pampeyan, E. H.: Buddingtonite in Menlo Park, California, U.S. Geological Survey Open-File Report 2010-1053, 10 pp., available at: http://pubs.usgs.gov/of/2010/1053/ (last access: 11 January 2022), 2010.
Patterson, J. H., Ramsden, A. R., and Dale, L. S.: Geochemistry and
mineralogical residences of trace elements in oil shales from the Condor
deposit, Queensland, Australia, Chem. Geol., 67, 327–340, 1988.
Pöter, B., Gottschalk, M., and Heinrich, W.: Crystal-chemistry of
synthetic K-feldspar-buddingtonite and muscovite-tobelite solid solutions,
Amer. Mineral., 92, 151–165, 2007.
Rainers, P. W. and Brandon, M. T.: Using thermochronology to understand
orogenic erosion, Ann. Rev. Earth Plant. Sci., 34, 419–466, 2006.
Ramseyer, K., Diamond, L. W., and Boles, J. R.: Authigenic
K-NH4-feldspar in sandstones: A fingerprint of the diagenesis of
organic matter, J. Sedim. Petrol., 63, 1092–1099, 1993.
Renne, P. R., Balco, G., Ludwig, K. R., Mundil, R., and Min, K.: Response to
the comment by W. H. Schwarz et al. on “Joint determination of 40K
decay constants and 40Ar*/40K for the Fish Canyon sanidine
standard, and improved accuracy for 40Ar/39Ar geochronology” by P. R. Renne et al. (2010), Geochim. Cosmochim. Acta, 75, 5097–5100, 2011.
Scibiorski, E., Jourdan, F., Mezger, K., Tohver, E., and Vollstaedt, H.:
Cryptic excess argon in metamorphic biotite: Anomalously old
40Ar/39Ar plateau dates tested with Rb Sr thermochronology and Ar diffusion modelling, Geochim. Cosmochim. Acta, 315, 1–23, 2021.
Shumlyanskyy, L., Hawkesworth, C., Dhuime, B,. Billström, K., Claesson,
S., and Storey, C.: 207Pb 206Pb ages and Hf isotope composition of zircons from sedimentary rocks of the Ukrainian shield: crustal growth of the south-western part of East European craton from Archaean to Neoproterozoic, Precam. Res., 260, 39–54, 2015.
Shumlyanskyy, L., Nosova, A., Billström, K., Söderlund, U.,
Andréasson, P.-G., and Kuzmenkova, O.: The U–Pb zircon and baddeleyite
ages of the Neoproterozoic Volyn Large Igneous Province: implication for the
age of the magmatism and the nature of a crustal contaminant, Gff Upsala,
138, 17–30, 2016.
Shumlyanskyy, L., Hawkesworth, C., Billström, K., Bogdanova, S.,
Mytrokhyn, O., Romer, R., Dhuime, B., Claesson, S., Ernst, R., Whitehouse,
M., and Bilan, O.: The origin of the Palaeoproterozoic AMCG complexes in the
Ukrainian shield: New U-Pb ages and Hf isotopes in zircon, Precam. Res.,
292, 216–239, 2017.
Shumlyanskyy, L., Franz, G., Glynn, S., Mytrokhyn, O., Voznyak, D., and Bilan, O.: Geochronology of granites of the western Korosten AMCG complex (Ukrainian Shield): implications for the emplacement history and origin of miarolitic pegmatites, Eur. J. Mineral., 33, 703–716, https://doi.org/10.5194/ejm-33-703-2021, 2021.
Solomon, G. C. and Rossman, G. R.: NH in pegmatitic feldspars
from the southern Black Hills, South Dakota, Amer. Mineral., 73, 818–821,
1988.
Steiger, R. H. and Jäger, E.: Subcommission on geochronology: Convention
on the use of decay constants in geo- and cosmochronology, Earth Planet.
Sci. Lett., 36, 359–362, 1977.
Svensen, H., Bebout, G., Kronz, A., Li, L., Planke, S., Chevallier, L., and
Jamtveit. B.: Nitrogen geochemistry as a tracer of fluid flow in a
hydrothermal vent complex in the Karoo Basin, South Africa, Geochim.
Cosmochim. Acta, 72, 4929–4947, 2008.
Uto, K., Ishizuka, O., Matsumoto, A., Kamioka, H., and Togashi, S.:
Laser-heating 40Ar/39Ar dating system of the Geological Survey of Japan: System outline and preliminary results, Bull. Geol. Surv. Japan, 48, 23–46, 1997.
Villa, I. M.: Advances in 40Ar/39Ar Dating: from Archaeology to Planetary Sciences, edited by: Jourdan, F., Mark, D. F., and Verati, C., Geol. Soc., London, Spec. Pub., 378, 107–116, 2014.
Villa, I. M., De Bièvre, P., Holden, N. E., and Renne, P. R.: IUPAC-IUGS
recommendation on the half-life of 87Rb, Geochim. Cosmochim. Acta, 164,
382–385, 2015.
Voncken, J. H. L., Van Roermund, H. L. M., Van der Eerden, A. M. J., Jansen,
J. B. H., and Erd, R. C.: Holotype buddingtonite: an ammonium feldspar
without zeolitic H2O, Amer. Mineral., 78, 204–209, 1993.
Voznyak, D. K., Khomenko, V. M., Franz, G., and Wiedenbeck, M.:
Physico-chemical conditions of the late stage Volyn pegmatite evolution:
Fluid inclusions in beryl studied by thermobarometry and IR-spectroscopy
methods, Mineral. J. (Ukraine), 34, 26–38, 2012.
Wartho, J., Kelley, S. P., Brooker, R. A., Carroll, M. R., Villa, I. M., and
Lee, M. R.: Direct measurement of Ar diffusion profiles in a gem-quality
Madagascar K-feldspar using the ultra-violet ablation microprobe (UVLAMP),
Earth Planet. Sci. Lett., 170, 141–153, 1999.
Zhmur, S. I.: Origin of Cambrian fibrous kerites of the Volyn region,
Lithol. Miner. Resour., 38, 55–73, 2003.
Short summary
The age of formation of buddingtonite, ammonium-bearing feldspar, can be dated with the Ar–Ar method; however, it may often give only minimum ages due to strong resetting. In the studied example it gives a Precambrian minimum age of fossils, associated with this occurrence, and the age of the accompanying mineral muscovite indicates an age near 1.5 Ga. We encourage more dating attempts of buddingtonite, which will give valuable information of diagenetic or hydrothermal events.
The age of formation of buddingtonite, ammonium-bearing feldspar, can be dated with the Ar–Ar...