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Broadmix Ergonomic High-densith Accent Chair with PU Leather Sea
Broadmix Ergonomic High-densith Accent Chair with PU Leather Sea
【Modern design】Human-oriented ergonomic construction offers a comfortable sitting experience. High-quality PU leather is waterproof and wear resistant, you could reused it for a long time.
【Stable and durable construction】Made of high quality steel frame, which could support 300lbs heavy weight. 360 degree swivel wheels with rubber casters make you move smoothly and quietly.
【Comfortable Design】High-density foam seat could support your lumbar and neck sufficiently, and meet your maximum comfort.
【Functions】High-back adjustable chair with a removeable lumbar cushion could meet your any need, you could ues it playing, working and other purposes.
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Adjustable angles could adjust to your any needs, and massage lumbar cushion could make you comfortable and feel better during working or playing games. The PU leather could make you reused it for a long time, and it is easy to clean.
Broadmix Ergonomic High-densith Accent Chair with PU Leather Sea
Eur. J. Mineral., 34, 183–200, https://doi.org/10.5194/ejm-34-183-2022,https://doi.org/10.5194/ejm-34-183-2022, 2022
The inclusions and exsolution lamellae in rainbow lattice sunstone (RLS) are studied using microscopic observations, chemical analyses and single-crystal X-ray diffraction. Complicated processes producing the aventurescence and adularescence effect in RLS are revealed through the spatial relationship among the inclusions and exsolution lamellae, as well as the unique ordering pattern in the feldspar structures.
Donato Belmonte, Mattia La Fortezza, and Francesca Menescardi
Eur. J. Mineral., 34, 167–182, https://doi.org/10.5194/ejm-34-167-2022,https://doi.org/10.5194/ejm-34-167-2022, 2022
We carried out theoretical calculations of the vibrational and thermophysical properties of Mg2SiO4 ringwoodite, a major mineral phase of the Earth's mantle transition zone. We tried to understand why current data on volume thermal expansion are still controversial by performing a detailed analysis of vibrational spectra. We proposed a reliable parametrization for thermal expansivity of ringwoodite in the transition zone which could be useful for numerical simulations of mantle convection.
Eur. J. Mineral., 34, 149–165, https://doi.org/10.5194/ejm-34-149-2022,https://doi.org/10.5194/ejm-34-149-2022, 2022
The previously unknown temperature gradient in Earth's largest layer is uniquely extracted from a seismology average, the only information available. Data used from laboratory studies are minimal and describe general behavior. Adding a new theory and data on heat transport properties provides flux (heat per area per time) and power (total wattage) vs. depth. Temperature vs. depth instead uses an additive constant, which is constrained by data on melting. I show the lower mantle is heating up.
Eur. J. Mineral., 34, 131–141, https://doi.org/10.5194/ejm-34-131-2022,https://doi.org/10.5194/ejm-34-131-2022, 2022
Vanadium carbides in shungite are shown to be present in several forms, which reflects the distinctive conditions of their formation. An ordered carbon film revealed on the vanadium carbide particles could protect the particles from transformations for a long time. The parageneses of vanadium carbide and roscoelite occur, indicating that roscoelite in shungite rocks may be a secondary mineral formed upon vanadium carbide decomposition.
Giulio Borghini, Patrizia Fumagalli, and Elisabetta Rampone
Eur. J. Mineral., 34, 109–129, https://doi.org/10.5194/ejm-34-109-2022,https://doi.org/10.5194/ejm-34-109-2022, 2022
The mineralogical and chemical heterogeneity of the mantle is poorly known because it is not able to be directly investigated. Melt–peridotite interaction processes play a fundamental role in controlling the mantle composition. The results of our reaction experiments help us to evaluate the role of temperature and melt composition in the modification of the mantle through the interaction with pyroxenite-derived melts with implications for the evolution of a veined mantle.
Yuan Xue, Ningyue Sun, Hongping He, Aiqing Chen, and Yiping Yang
Eur. J. Mineral., 34, 95–108, https://doi.org/10.5194/ejm-34-95-2022,https://doi.org/10.5194/ejm-34-95-2022, 2022
Liguowuite, a new member of the non-stoichiometric perovskite group minerals, ideally WO3, has been found in the Panzhihua–Xichang region, China. Liguowuite is monoclinic and is in space group P21 / n, with a = 7.32582(18) Å, b = 7.54767(18) Å, c = 7.71128(18) Å, β = 90.678(3)°, V = 426.348(19) Å3, and Z = 8. According to the hierarchical scheme for perovskite supergroup minerals, liguowuite is the first reported example of A-site vacant single oxide, i.e., a new perovskite subgroup.
Eur. J. Mineral., 34, 85–94, https://doi.org/10.5194/ejm-34-85-2022,https://doi.org/10.5194/ejm-34-85-2022, 2022
The École des Mines de Saint-Étienne possesses an important collection of wooden crystallographic models. Rehabilitation action was undertaken. Several series of Krantz models were identified by the logos and linked to catalogs. An exceptional element was discovered: a polyhedron with 170 facets, from the cubic system. We report on the digitalization work, followed by a description of two duplication methods: 3D printing and precision lost-wax vacuum casting.
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Nicolas Tribovillard, Viviane Bout-Roumazeilles, Marion Delattre, Sandra Ventalon, and Abderrahmane Bensadok
Eur. J. Mineral., 34, 77–83, https://doi.org/10.5194/ejm-34-77-2022,https://doi.org/10.5194/ejm-34-77-2022, 2022
The studied succession of limestone and marls is enriched in pyrite framboids. The question is, could sulfate-reducing bacteria have been trapped in pyrite sarcophagi induced by their own metabolism? Our analysis reveals the presence of abundant organic matter. The typical morphology of framboids suggests the early fossilization of bacterial colonies by pyrite. If pyrite is a trap for organic molecules, then pyrite could be an underevaluated component of the C cycle.
Carla Tiraboschi, Francesca Miozzi, and Simone Tumiati
Eur. J. Mineral., 34, 59–75, https://doi.org/10.5194/ejm-34-59-2022,https://doi.org/10.5194/ejm-34-59-2022, 2022
This review provides an overview of ex situ carbon-saturated COH fluid experiments at upper-mantle conditions. Several authors experimentally investigated the effect of COH fluids. However, fluid composition is rarely tackled as a quantitative issue, and rather infrequently fluids are analyzed as the associated solid phases in the experimental assemblage. Recently, improved techniques have been proposed for analyses of COH fluids, leading to significant advancement in fluid characterization.
Enrico Cannaò, Massimo Tiepolo, Giulio Borghini, Antonio Langone, and Patrizia Fumagalli
Eur. J. Mineral., 34, 35–57, https://doi.org/10.5194/ejm-34-35-2022,https://doi.org/10.5194/ejm-34-35-2022, 2022
Amphibole–liquid partitioning of elements of geological relevance is experimentally derived at conditions compatible with those of the Earth's upper mantle. Experiments are carried out at different oxygen fugacity conditions and variable Cl content in order to investigate their influence on the amphibole–liquid partition coefficients. Our results point to the capability of amphibole to act as filter for trace elements at upper-mantle conditions, oxidized conditions, and Cl-rich environments.
Eur. J. Mineral., 34, 19–34, https://doi.org/10.5194/ejm-34-19-2022,https://doi.org/10.5194/ejm-34-19-2022, 2022
Detailed knowledge of the mechanisms ruling water incorporation in amphibole is essential to understand how much water can be fixed at upper-mantle conditions by this mineral. We provide the experimental evidence of the Cl effect on the oxo-substitution and the incorporation of water in amphibole. Finally, we highlight the versatility of confocal micro-Raman spectroscopy as an analytical tool to quantify water in amphibole.
Gerhard Franz, Masafumi Sudo, and Vladimir Khomenko
Eur. J. Mineral., 34, 7–18, https://doi.org/10.5194/ejm-34-7-2022,https://doi.org/10.5194/ejm-34-7-2022, 2022
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.