Articles | Volume 33, issue 5
https://doi.org/10.5194/ejm-33-571-2021
© Author(s) 2021. 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-33-571-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
24 Sep 2021
Research article |
| 24 Sep 2021
| 24 Sep 2021
Uniform “water” content in quartz phenocrysts from silicic pyroclastic fallout deposits – implications on pre-eruptive conditions
ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Physical Geography,
Pázmány Péter sétány 1/C, 1117, Budapest, Hungary
Tamás Biró
ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Physical Geography,
Pázmány Péter sétány 1/C, 1117, Budapest, Hungary
István János Kovács
MTA EK Lendület Pannon LitHOscope Research Group,
Konkoly-Thege Miklós út 29-33, 1121, Budapest, Hungary
Roland Stalder
Institute of Mineralogy and Petrography, University of Innsbruck,
Innrain 52f, 6020, Innsbruck, Austria
Károly Németh
School of Agriculture and Environment, Massey University, Private Bag
11, 222 Palmerston North, 4442, New Zealand
Institute of Earth Physics and Space Sciences, Csatkai E. u. 6-8,
Sopron, 9400, Hungary
Alexandru Szakács
Department of Endogene
Processes, Natural Hazard and Risk, Romanian Academy, Institute of Geodynamics, 19-21 Jean-Louis Calderon St., 020032,
Bucharest-37, Romania
Zsófia Pálos
Department of Earth Sciences, Mineral Resources
and Geofluids Group, University of Geneva, 13, Rue des Maraîchers, 1205 Geneva, Switzerland
Zoltán Pécskay
Institute of Nuclear Research (ATOMKI), Isotope Climatology and
Environmental Research Centre (ICER), K-Ar Group, Bem tér 18/c, 4026,
Debrecen, Hungary
Dávid Karátson
ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Physical Geography,
Pázmány Péter sétány 1/C, 1117, Budapest, Hungary
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Roland Stalder
Eur. J. Mineral., 33, 145–163, https://doi.org/10.5194/ejm-33-145-2021, https://doi.org/10.5194/ejm-33-145-2021, 2021
Short summary
Short summary
Hydrous defects in quartz contain important information regarding the origin and history of individual grains. This article summarises the findings from experimental work and analysis of natural material over the past 60 years, and results are interpreted with respect to igneous, metamorphic, and sedimentary processes.
Eszter Szűcs, Sándor Gönczy, István Bozsó, László Bányai, Alexandru Szakacs, Csilla Szárnya, and Viktor Wesztergom
Nat. Hazards Earth Syst. Sci., 21, 977–993, https://doi.org/10.5194/nhess-21-977-2021, https://doi.org/10.5194/nhess-21-977-2021, 2021
Short summary
Short summary
Sinkhole formation and post-collapse deformation in the Solotvyno salt mining area was studied where the salt dissolution due to water intrusion poses a significant risk. Based on a Sentinel-1 data set, remarkable surface deformation with a maximum rate of 5 cm/yr was revealed, and it was demonstrated that the deformation process has a linear characteristic although the mining activity was ended more than 10 years ago.
Related subject area
Defects in minerals and phase transitions
Defects in olivine
OH point defects in quartz – a review
Partitioning of chromium between garnet and clinopyroxene: first-principle modelling versus metamorphic assemblages
Sylvie Demouchy
Eur. J. Mineral., 33, 249–282, https://doi.org/10.5194/ejm-33-249-2021, https://doi.org/10.5194/ejm-33-249-2021, 2021
Short summary
Short summary
Olivine, a ferromagnesian orthosilicate, is the most abundant mineral in Earth’s upper mantle but also in Mars' and Venus'. The olivine atomic structure is also used to manufacture lithium batteries. Like any other crystalline solid, olivine never occurs with a perfect crystalline structure: defects in various dimensions are ubiquitous. In this contribution, I review the current state of the art of defects in olivine and several implications for key processes in geodynamics.
Roland Stalder
Eur. J. Mineral., 33, 145–163, https://doi.org/10.5194/ejm-33-145-2021, https://doi.org/10.5194/ejm-33-145-2021, 2021
Short summary
Short summary
Hydrous defects in quartz contain important information regarding the origin and history of individual grains. This article summarises the findings from experimental work and analysis of natural material over the past 60 years, and results are interpreted with respect to igneous, metamorphic, and sedimentary processes.
Sarah Figowy, Benoît Dubacq, Yves Noël, and Philippe d'Arco
Eur. J. Mineral., 32, 387–403, https://doi.org/10.5194/ejm-32-387-2020, https://doi.org/10.5194/ejm-32-387-2020, 2020
Short summary
Short summary
Partition coefficients are key to petrological modelling yet hard to estimate independently of measurements. Here we model the partitioning of Cr between garnet and clinopyroxene ab initio. Incorporation of Cr into crystal structures causes strain, and its energetic toll defines whether Cr favours one mineral or another. Comparing to Cr content in metamorphic rocks shows how mineral composition and structure set equilibrium partition coefficients and how kinetics hampers equilibrium.
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Short summary
We sampled pyroclastic fallout deposits from Hungary and from New Zealand in order to get the original
watercontent of the quartz crystals. Our main results imply no significant change in water content of the quartz phenocrysts. All sampled crystal populations contain identical water contents in case of both the Bükk Foreland and the Kaharoa eruption. Thus, there may have been similar physicochemical conditions in the magmatic system just before the eruption.
We sampled pyroclastic fallout deposits from Hungary and from New Zealand in order to get the...
