Articles | Volume 35, issue 3
https://doi.org/10.5194/ejm-35-361-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/ejm-35-361-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 May 2023
Research article |
| 31 May 2023
| 31 May 2023
In situ single-crystal X-ray diffraction of olivine inclusion in diamond from Shandong, China: implications for the depth of diamond formation
Yanjuan Wang
Department of Geosciences, University of Padua, Padua, 35131, Italy
School of Earth Sciences and Resources, China University of
Geosciences, Beijing, 100083, China
Fabrizio Nestola
CORRESPONDING AUTHOR
Department of Geosciences, University of Padua, Padua, 35131, Italy
Huaikun Li
Tianjin Center, China Geological Survey, Tianjin, 300171, China
Zengqian Hou
School of Earth Sciences and Resources, China University of
Geosciences, Beijing, 100083, China
Martha G. Pamato
Department of Geosciences, University of Padua, Padua, 35131, Italy
Davide Novella
Department of Geosciences, University of Padua, Padua, 35131, Italy
Alessandra Lorenzetti
Department of Industrial Engineering, University of Padua, Padua,
35131, Italy
Pia Antonietta Antignani
Italian Gemmology Laboratory, LabiGem, Vicenza, 36100, Italy
Paolo Cornale
Italian Gemmology Laboratory, LabiGem, Vicenza, 36100, Italy
Jacopo Nava
Department of Geosciences, University of Padua, Padua, 35131, Italy
Guochen Dong
School of Earth Sciences and Resources, China University of
Geosciences, Beijing, 100083, China
Tianjin Center, China Geological Survey, Tianjin, 300171, China
School of Earth Sciences and Engineering, Nanjing University, Nanjing,
210023, China
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Bobtraillite is an extremely rare cyclosilicate with a unique composition and complex structure. In this paper, we describe the second occurrence of the extremely rare complex zirconium silicate. The results suggest that the ideal formula of bobtraillite could be written as (Na, □)12(□, Na)12Sr12Zr14(Si3O9)10[Si2BO7(OH)2]6·12H2O.
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Kai Qu, Xianzhang Sima, Xiangping Gu, Weizhi Sun, Guang Fan, Zeqiang Yang, and Yanjuan Wang
Eur. J. Mineral., 36, 397–409, https://doi.org/10.5194/ejm-36-397-2024, https://doi.org/10.5194/ejm-36-397-2024, 2024
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In this paper, the full description of the extremely rare [Ag6]4+-cluster-containing new tetrahedrite-group mineral kenoargentotetrahedrite-(Zn) is reported. The structure refinement result confirms the coupling between the site occupancy factor of subvalent hexasilver clusters at the M(2) site and that of the vacancy at the S(2) site. This relationship further substantiates the charge balance substitution mechanism of S-deficiency tetrahedrites: 6M(2)Ag+ + S(2)S2– = M(2)[Ag6]4+ + S(2)□.
Daniel Atencio, Andrezza A. Azzi, Kai Qu, Ritsuro Miyawaki, Ferdinando Bosi, and Koichi Momma
Eur. J. Mineral., 35, 1027–1030, https://doi.org/10.5194/ejm-35-1027-2023, https://doi.org/10.5194/ejm-35-1027-2023, 2023
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This article introduces a new nomenclature system for the cerite group minerals. This system was necessary to allow the nomenclature of new species of minerals that are currently being described.
Jiří Sejkora, Cristian Biagioni, Pavel Škácha, Silvia Musetti, Anatoly V. Kasatkin, and Fabrizio Nestola
Eur. J. Mineral., 35, 897–907, https://doi.org/10.5194/ejm-35-897-2023, https://doi.org/10.5194/ejm-35-897-2023, 2023
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We present the description of new mineral – a Cd-dominant member of the tetrahedrite group, tetrahedrite-(Cd), from the Radětice deposit near Příbram, Czech Republic. All necessary data including crystal structure were successfully determined, and the mineral and its name have been approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (number 2022-115).
Ross J. Angel, Mattia L. Mazzucchelli, Kira A. Musiyachenko, Fabrizio Nestola, and Matteo Alvaro
Eur. J. Mineral., 35, 461–478, https://doi.org/10.5194/ejm-35-461-2023, https://doi.org/10.5194/ejm-35-461-2023, 2023
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Yanjuan Wang, Fabrizio Nestola, Zengqian Hou, Xiangping Gu, Guochen Dong, Zhusen Yang, Guang Fan, Zhibin Xiao, and Kai Qu
Eur. J. Mineral., 35, 65–74, https://doi.org/10.5194/ejm-35-65-2023, https://doi.org/10.5194/ejm-35-65-2023, 2023
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Bobtraillite is an extremely rare cyclosilicate with a unique composition and complex structure. In this paper, we describe the second occurrence of the extremely rare complex zirconium silicate. The results suggest that the ideal formula of bobtraillite could be written as (Na, □)12(□, Na)12Sr12Zr14(Si3O9)10[Si2BO7(OH)2]6·12H2O.
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Claudia Agnini, Martha G. Pamato, Gabriella Salviulo, Kim A. Barchi, and Fabrizio Nestola
Adv. Geosci., 53, 155–167, https://doi.org/10.5194/adgeo-53-155-2020, https://doi.org/10.5194/adgeo-53-155-2020, 2020
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This work provides updated scenario on the underrepresentation of women in the Italian university system in the area of geosciences in the last two decades. Data highlight an increase in the number of female full and associate professors whereas the low number of female non-permanent researchers raises strong concerns. Over different areas of geosciences, Paleontology represents the only field in which the gap is filled whereas all the other disciplines suffer a gender imbalance.
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A brief history of solid inclusion piezobarometry
Li–Na interdiffusion and diffusion-driven lithium isotope fractionation in pegmatitic melts
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Benjamin A. Pummell and Jay B. Thomas
Eur. J. Mineral., 36, 581–597, https://doi.org/10.5194/ejm-36-581-2024, https://doi.org/10.5194/ejm-36-581-2024, 2024
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Mechanical interaction between quartz inclusions in garnet creates residual pressure in the inclusion used to calculate the pressure and temperature where the two minerals formed. We crystallised quartz and garnet at high pressure and temperature and then adjusted the experimental pressure to observe the interaction between the quartz inclusions and garnet host. The quartz and garnet adjust to the new experimental pressures, reset inclusion pressures, and no longer match entrapment conditions.
Colin Fauguerolles, Teddy Castelain, Johan Villeneuve, and Michel Pichavant
Eur. J. Mineral., 36, 555–579, https://doi.org/10.5194/ejm-36-555-2024, https://doi.org/10.5194/ejm-36-555-2024, 2024
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To explore the influence of the redox state of the environment on the serpentinization reaction, we have developed an original experimental setup. Reducing conditions, leading to the formation of serpentine and magnetite, and oxidizing conditions, leading to the formation of serpentine and hematite, are discussed in terms of analogues of low- and high-permeability hydrothermal systems, respectively. The influence of the redox on brucite stability and hydrogen production is also established.
Ross J. Angel, Matteo Alvaro, and Silvio Ferrero
Eur. J. Mineral., 36, 411–415, https://doi.org/10.5194/ejm-36-411-2024, https://doi.org/10.5194/ejm-36-411-2024, 2024
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Inclusions in natural rocks are an invaluable asset for geoscientists because they provide information about processes in the Earth's history that are otherwise hidden or subsequently overprinted. In this paper we review the development over the last 200 years of the concepts and methods to measure the remnant pressures in mineral inclusions and how they can be used to determine pressures and temperatures at which the inclusions were formed deep within the Earth.
Christian R. Singer, Harald Behrens, Ingo Horn, Martin Oeser, Ralf Dohmen, and Stefan Weyer
Eur. J. Mineral., 35, 1009–1026, https://doi.org/10.5194/ejm-35-1009-2023, https://doi.org/10.5194/ejm-35-1009-2023, 2023
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Li is a critical element that is often enriched in pegmatites. To better understand the enrichment of Li in such systems, it is necessary to understand the underlying transport mechanisms. We performed experiments to investigate diffusion rates and exchange mechanisms of Li between a Li-rich and a Li-poor melt at high temperature and pressure. Our results indicate that fluxing elements do not increase the diffusivity of Li compared to a flux-free melt.
Martin Oeser, Ingo Horn, Ralf Dohmen, and Stefan Weyer
Eur. J. Mineral., 35, 813–830, https://doi.org/10.5194/ejm-35-813-2023, https://doi.org/10.5194/ejm-35-813-2023, 2023
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This study presents a new method designed to analyze micrometer-scale chemical and isotopic profiles in minerals, glasses, and other solids. The employed technique combines plasma mass spectrometers and a state-of-the-art femtosecond laser equipped with open-source software (LinuxCNC) that controls the movement of the laser beam. It allows for equably drilling into the sample surface, e.g., in order to measure chemically or isotopically zoned or heterogeneous materials at micrometer scales.
Marc M. Hirschmann and Hongluo L. Zhang
Eur. J. Mineral., 35, 789–803, https://doi.org/10.5194/ejm-35-789-2023, https://doi.org/10.5194/ejm-35-789-2023, 2023
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We calibrate new models for the properties of solid and liquid FePt alloy. FePt alloy is used in experiments investigating the origin, differentiation, and evolution of planets to characterize oxygen fugacity. The new models facilitate use of FePt for more extreme conditions than has been possible previously. We also describe shortcomings in the present knowledge of FePt alloy properties and highlight strategies that could improve such knowledge.
Ross J. Angel, Mattia L. Mazzucchelli, Kira A. Musiyachenko, Fabrizio Nestola, and Matteo Alvaro
Eur. J. Mineral., 35, 461–478, https://doi.org/10.5194/ejm-35-461-2023, https://doi.org/10.5194/ejm-35-461-2023, 2023
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We have developed the thermodynamic theory of the properties of inclusions consisting of more than one phase, including inclusions containing solids plus a fluid. We present a software utility that enables for the first time the entrapment conditions of multiphase inclusions to be determined from the measurement of their internal pressure when that is measured in a laboratory.
Shashank Prabha-Mohan, Kenneth T. Koga, Antoine Mathieu, Franck Pointud, and Diego F. Narvaez
Eur. J. Mineral., 35, 321–331, https://doi.org/10.5194/ejm-35-321-2023, https://doi.org/10.5194/ejm-35-321-2023, 2023
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This work presents an in-depth description of a new design for a high-temperature gas-mixing furnace using a mixture of CO–CO2–SO2. It has been designed and built with user safety in mind. The furnace can sustain temperatures of up to 1650 °C. This furnace sets itself apart with its size and unique quench mechanism. Crucially, the apparatus has the ability to change the gas mixture during an experiment. This feature allows the user to simulate natural environments, such as volcanoes.
Lennart Koch and Burkhard C. Schmidt
Eur. J. Mineral., 35, 117–132, https://doi.org/10.5194/ejm-35-117-2023, https://doi.org/10.5194/ejm-35-117-2023, 2023
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Volatile diffusivities in silicate melts control the nucleation and growth of bubbles in ascending magma. We investigated the diffusion of CO2 in an anhydrous and hydrous leucititic melt at high temperatures and high pressure. CO2 diffusion profiles were measured via attenuated total reflection Fourier transform infrared spectroscopy. CO2 diffusion increases with increasing temperature and water content. The data can be used to understand the CO2 degassing behaviour of leucititic melts.
Melanie J. Sieber, Max Wilke, Oona Appelt, Marcus Oelze, and Monika Koch-Müller
Eur. J. Mineral., 34, 411–424, https://doi.org/10.5194/ejm-34-411-2022, https://doi.org/10.5194/ejm-34-411-2022, 2022
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Carbonates reduce the melting point of the mantle, and carbonate melts produced in low-degree melting of a carbonated mantle are considered the precursor of CO2-rich magmas. We established experimentally the melting relations of carbonates up to 9 GPa, showing that Mg-carbonates melt incongruently to periclase and carbonate melt. The trace element signature of carbonate melts parental to kimberlites is approached by melting of Mg-rich carbonates.
Roxane Buso, Didier Laporte, Federica Schiavi, Nicolas Cluzel, and Claire Fonquernie
Eur. J. Mineral., 34, 325–349, https://doi.org/10.5194/ejm-34-325-2022, https://doi.org/10.5194/ejm-34-325-2022, 2022
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Magmas transport large amounts of CO2 from Earth's mantle into the atmosphere and thus contribute significantly to the global carbon cycle. We have developed an experimental method to homogenize at high pressure small liquid droplets trapped in magmatic crystals to gain access to the initial composition of the parental magma (major and volatile elements). With this technique, we show that magmas produced by melting of the subcontinental mantle contain several weight percent of CO2.
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
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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
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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.
Enrico Cannaò, Federica Schiavi, Giulia Casiraghi, Massimo Tiepolo, and Patrizia Fumagalli
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
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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.
Michael C. Jollands, Hugh St.C. O'Neill, Andrew J. Berry, Charles Le Losq, Camille Rivard, and Jörg Hermann
Eur. J. Mineral., 33, 113–138, https://doi.org/10.5194/ejm-33-113-2021, https://doi.org/10.5194/ejm-33-113-2021, 2021
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How, and how fast, does hydrogen move through crystals? We consider this question by adding hydrogen, by diffusion, to synthetic crystals of olivine doped with trace amounts of chromium. Even in a highly simplified system, the behaviour of hydrogen is complex. Hydrogen can move into and through the crystal using various pathways (different defects within the crystal) and hop between these pathways too.
Joana Polednia, Ralf Dohmen, and Katharina Marquardt
Eur. J. Mineral., 32, 675–696, https://doi.org/10.5194/ejm-32-675-2020, https://doi.org/10.5194/ejm-32-675-2020, 2020
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Grain boundary diffusion is orders of magnitude faster compared to volume diffusion. We studied this fast transport process in a well-defined garnet grain boundary. State-of-the-art microscopy was used for quantification. A dedicated numerical diffusion model shows that iron diffusion requires the operation of two diffusion modes, one fast, one slow. We conclude that impurity bulk diffusion in garnet aggregates is always dominated by grain boundary diffusion.
Giulio Borghini and Patrizia Fumagalli
Eur. J. Mineral., 32, 251–264, https://doi.org/10.5194/ejm-32-251-2020, https://doi.org/10.5194/ejm-32-251-2020, 2020
Alan B. Woodland, Andrei V. Girnis, Vadim K. Bulatov, Gerhard P. Brey, and Heidi E. Höfer
Eur. J. Mineral., 32, 171–185, https://doi.org/10.5194/ejm-32-171-2020, https://doi.org/10.5194/ejm-32-171-2020, 2020
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We experimentally explored direct entrapment of breyite (CaSiO3) by diamond at upper-mantle conditions in a model subducted sediment rather than formation by retrogression of CaSiO3 perovskite, implying a deeper origin. Anhydrous low-T melting of CaCO3+SiO2 precludes breyite formation. Under hydrous conditions, reduction of melt results in graphite with breyite. Thus, breyite inclusions in natural diamond may form from aragonite + coesite or carbonate melt at 6–8 GPa via reduction with water.
Cited articles
Angel, R. J. and Nestola, F.: A century of mineral structures: How well do
we know them?, Am. Mineral., 101, 1036–1045, 2016.
Angel, R. J., Mazzucchelli, M. L., Alvaro, M., Nimis, P., and Nestola, F.:
Geobarometry from host-inclusion systems: The role of elastic relaxation,
Am. Mineral., 99, 2146–2149, 2014.
Angel, R. J., Alvaro, M., Nestola, F., and Mazzucchelli, M. L.: Diamond
thermoelastic properties and implications for determining the pressure of
formation of diamond-inclusion systems, Russ. Geol. Geophys., 56, 211–220,
2015.
Angel, R. J., Mazzucchelli, M. L., Alvaro, M., and Nestola, F.: EosFit-Pinc:
A simple GUI for host–inclusion elastic thermobarometry, Am. Mineral., 102,
1957–1960, 2017.
Angel, R. J., Alvaro, M., and Nestola, F.: 40 years of mineral elasticity: a
critical review and a new parameterisation of equations of state for mantle
olivines and diamond inclusions, Phys. Chem. Miner., 45, 95–113, 2018a.
Angel, R. J., Murri, M., Mihailova, B., and Alvaro, M.: Stress, strain and
Raman shifts, Z. Kristallogr. Cryst. Mater., 234, 129–140, 2018b.
Angel, R. J., Alvaro, M., and Nestola, F.: Crystallographic methods for
non-destructive characterization of mineral inclusions in diamonds, Rev.
Mineral. Geochem., 88, 257–305, 2022.
Angel, R. J., Mazzucchelli, M., Kira, A. Musiyachenko, K. A., Nestola, F.,
and Alvaro, M.: Elasticity of mixtures and implications for piezobarometry
of mixed-phase inclusions, Eur. J. Mineral., in press, 2023.
Boyd, S. R., Kiflawi, I., and Woods, G. S.: The relationship between
infrared absorption and the A defect concentration in diamond, Philos. Mag.,
69, 1149–1153, 1994.
Boyd, S. R., Kiflawi, I., and Woods, G. S.: Infrared absorption by the B
nitrogen aggregate in diamond, Philos. Mag., 72, 351–361, 1995.
Breeding, C. M. and Shigley, J. E.: The “type” classification system of
diamonds and its importance in gemology, Gems. Gemol., 45, 96–111, 2009.
Bussweiler, Y., Brey, G. P., Pearson, D. G., Stachel, T., Stern, R. A.,
Hardman, M. F., Kjarsgaard B. A., and Jackson, S. E.: The
aluminum-in-olivine thermometer for mantle peridotites – Experimental versus
empirical calibration and potential applications, Lithos, 272, 301–314,
2017.
Chi, J. S. and Lu, F. X.: Kimberlite and Palaeozoic Lithospheric mantle in
North China Platform, Beijing, Science Press, ISBN: 7-03-005189-0, 1996.
Chrenko, R. M., Tuft, R. E., and Strong, H. M.: Transformation of the state
of nitrogen in diamond, Nature, 270, 141–144, 1977.
Day, H. W.: A revised diamond-graphite transition curve, Am. Mineral., 97,
52–62, 2012.
Faccincani, L., Cerantola, V., Nestola, F., Nimis, P., Ziberna, L., Pasqualetto, L., Chumakov, A. I., Harris, J. W., and Coltorti, M.: Relatively oxidized conditions for diamond formation at Udachnaya (Siberia), Eur. J. Mineral., 34, 549–561, https://doi.org/10.5194/ejm-34-549-2022, 2022.
Farrugia, L. J.: WinGX and ORTEP for Windows: an update, J. Appl.
Crystallogr., 45, 849–854, 2012.
Gonzalez-Platas, J., Alvaro, M., Nestola, F., and Angel, R. J.: EosFit7-GUI:
A new GUI tool for equation of state calculations, analyses and teaching, J.
Appl. Crystallogr., 49, 1377–1382, 2016.
Griffin, W. L., Zhang, A., O'Reilly, S. Y., and Ryan, C. G.: Phanerozoic
evolution of the lithosphere beneath the Sino-Korean craton, in: Mantle dynamics and plate
interactions in eastern Asia, edited by: Flower, M.,
Chung, S. L., Lo, C. H., and Lee, Y. Y., Washington, DC, American Geophysical Union,
Geodynamics Series, 27, 107–126, ISBN: 0875905293, 1998.
Hasterok, D. and Chapman, D. S.: Heat production and geotherms for the
continental lithosphere, Earth Planet. Sc. Lett., 307, 59–70, 2011.
Howell, D., Wood, I. G., Nestola, F., Nimis, P., and Nasdala, L.: Inclusions
under remnant pressure in diamond: a multi-technique approach, Eur. J.
Mineral., 24, 563–573, 2012.
Izraeli, E. S., Harris, J. W., and Navon, O.: Raman barometry of diamond
formation, Earth Planet. Sc. Lett., 173, 351–360, 1999.
Karaevangelou, M., Kopylova, M. G., Luo, Y., Pearson, D. G., Reutsky, V. N.,
and Loudon, P.: Mineral inclusions in Lace diamonds and the mantle beneath
the Kroonstad kimberlite cluster in South Africa, Contrib. Mineral. Petrol.,
177, 20, https://doi.org/10.1007/s00410-021-01880-8, 2022.
Korolev, N., Kopylova, M., Gurney, J. J., Moore, A. E., and Davidson, J.:
The origin of Type II diamonds as inferred from Cullinan mineral inclusions,
Miner. Petrol., 112, 275–289, 2018.
Leahy, K. and Taylor, W. R.: The influence of the Glennie domain deep structure on the diamonds in Saskatchewan kimberlites, Geol. Geofiz., 38, 451–460, 1997.
Li, Q. L., Wu, F. Y., Li, X. H., Qiu, Z. L., Liu, Y., Yang, Y. H., and Tang,
G. Q.: Precisely dating Paleozoic kimberlites in the North China Craton and
Hf isotopic constraints on the evolution of the subcontinental lithospheric
mantle, Lithos, 126, 127–134, 2011.
Liu, D. Y., Nutman, A. P., Compston, W., Wu, J. S., and Shen, Q. H.:
Remnants of ≥ 3800 Ma crust in the Chinese part of the Sino-Korean
Craton, Geology, 20, 339–342, 1992.
Mazzucchelli, M. L., Burnley, P., Angel, R. J., Morganti, S., Domeneghetti,
M. C., Nestola, F., and Alvaro, M.: Elastic geothermobarometry: Corrections
for the geometry of the host-inclusion system, Geology, 46, 231–234, 2018.
Mazzucchelli, M. L., Angel, R. J., and Alvaro, M.: EntraPT: an online
platform for elastic geothermobarometry, Am. Mineral., 106, 830–837, 2021.
Nestola, F., Nimis, P., Ziberna, L., Longo, M., Marzoli, A., Harris, J. W.,
Manghnani, M. H., and Fedortchouk, Y.: First crystal-structure determination
of olivine in diamond: Composition and implications for provenance in the
Earth's mantle, Earth Planet. Sc. Lett., 305, 249–255, 2011a.
Nestola, F., Pasqual, D., Smyth, J. R., Novella, D., Secco, L., Manghnani,
M. H., and Dal Negro, A.: New accurate elastic parameters for the
forsterite-fayalite solid solution, Am. Mineral., 96, 1742–1747, 2011b.
Nestola, F., Prencipe, M., Nimis, P., Sgreva, N., Perritt, S. H., Chinn, I.
L., and Zaffiro, G.: Toward a robust elastic geobarometry of kyanite
inclusions in eclogitic diamonds, J. Geophys. Res.-Sol. Ea., 123,
6411–6423, 2018.
Nestola, F., Zaffiro, G., Mazzucchelli, M. L., Nimis, P., Andreozzi, G. B.,
Periotto, B., Princivalle, F., Lenaz, D., Secco, L., Pasqualetto, L.,
Logvinova, A. M., Sobolev, N. V., Lorenzetti, A., and Harris, J. W.:
Diamond-inclusion system recording old deep lithosphere conditions at
Udachnaya (Siberia), Sci. Rep., 9, 1–8, 2019.
Ni, P. and Zhu, R. Z.: Evaluating the diamond potential of kimberlite-hosted
diamond deposits from the North China Craton, Acta Geol. Sin., 94,
2557–2573, 2020.
Nimis, P.: Pressure and temperature data for diamonds, in: Reviews in
Mineralogy and Geochemistry, edited by: Smit, K., Shirey, S., Pearson, G., Stachel,
T., Nestola, F., and Moses, T., Min. Soc. Am. And Geochem. Soc.,
Washington, 88, 533–566, 2022.
Nimis, P. and Taylor, W. R.: Single clinopyroxene thermobarometry for garnet
peridotites, Part I. Calibration and testing of a Cr-in-Cpx barometer and an
enstatite-in-Cpx thermometer, Contrib. Mineral. Petrol., 139, 541–554,
2000.
Nimis, P., Alvaro, M., Nestola, F., Angel, R. J., Marquardt, K., Rustioni,
G., and Harris, J. W.: First evidence of hydrous silicic fluid films around
solid inclusions in gem-quality diamonds, Lithos, 260, 384–389, 2016.
Nimis, P., Perritt S. H., and Ingrid C.: Diamond's depth distribution
systematics, Lithos, 376/377, 105729, https://doi.org/10.1016/j.lithos.2020.105729, 2020.
Poe, B. T., Romano, C., Nestola, F., and Smyth, J. R.: Electrical
conductivity anisotropy of dry and hydrous olivine at 8 GPa, Phys. Earth
Planet. Inter., 181, 103–111, 2010.
Rigaku Oxford Diffraction.: CrysAlisPro Software system, version 42.23a,
Rigaku Corporation, https://www.rigaku.com/products/crystallography/crysalis (last access: 30 May 2023), 2021.
Sheldrick, G. M.: SHELXT–Integrated space-group and crystal structure
determination, Ac. Crystallogr. C, 71, 3–8, 2015.
Smit, K. V., Timmerman, S., Aulbach, S., Shirey, S. B., Richardson, S. H.,
Phillips, D., and Pearson, D. G.: Geochronology of diamonds, Rev. Mineral.
Geochem., 88, 567–636, 2022.
Stachel, T., Harris, J. W.: The origin of cratonic diamonds-Constraints from
mineral inclusions, Ore Geol. Rev., 34, 5–32, 2008.
Stachel, T., Aulbach, S., and Harris, J. W.: Mineral inclusions in
lithospheric diamonds, Rev. Mineral. Geochem., 88, 307–392, 2022.
Taylor, W. R., Jaques, A. L., and Ridd, M.: Nitrogen-defect aggregation
characteristics of some Australasian diamonds; time-temperature constraints
on the source regions of pipe and alluvial diamonds, Am. Mineral., 75,
1290–1310, 1990.
Wilson, A. J. C.: International Tables for
Crystallography, edited by: Wilson, A. J. C., Kluwer Academic Publishers, Dordrecht, Vol. C, ISBN: 0792329503, 1995.
Wu, F. Y., Walker, R. J., Ren, X. W., Sun, D. Y., and Zhou, X. H.: Osmium
isotopic constraints on the age of lithospheric mantle beneath northeastern
China, Chem. Geol., 197, 107–129, 2003.
Wu, F. Y., Zhao, G. C., Wilde, S. A., and Sun, D. Y.: Nd Isotopic
constraints on the crustal formation of the North China Craton, Asian J.
Earth Sci., 24, 523–545, 2005.
Wu, F. Y., Zhang, Y. B., Yang, J. H., Xie, L. W., and Yang, Y. H.: Zircon
U–Pb and Hf isotopic constraints on the Early Archean crustal evolution of
the North China Craton, Precambrian Res., 167, 339–362, 2008.
Wu, G. C., Yu, X. Y., Liu, F., Li, H. B., Long, Z. Y., and Wang, H.: Color
Genesis of Brown Diamond from the Mengyin Kimberlite, China, Crystals, 12,
449, https://doi.org/10.3390/cryst12040449, 2022.
Yang, Y. H., Wu, F. Y., Wilde, S. A., Liu, X. M., Zhang, Y. B., Xie, L. W.,
and Yang, J. H.: In situ perovskite Sr–Nd isotopic constraints on the
petrogenesis of the Ordovician Mengyin kimberlites in the North China
Craton, Chem. Geol., 264, 24–42, 2009.
Yin, L., Zhang, R. S., and Zheng, J. P.: Mineral chemistry characters of
diamond inclusions and the nature of the lithospheric mantle beneath the
eastern North China Craton, Geo. Sci. Tech. Info., 25, 21–28, 2008 (in
Chinese with English abstract).
Yin, Z. W., Lu, F. X., Chen, M. H., and Xu, H. Y.: Ages and environments of
formation of diamonds in Mengyin County, Shandong Province, Earth Sci.
Front., 12, 614–621, 2005 (in Chinese with English abstract).
Yin, Z. W., Jiang, C., Chen, M. H., Lu, F. X., and Chen, Q.: Inclusions of
α-quartz, albite and olivine in a mantle diamond, Gondwana Res., 44,
228–235, 2017.
Zhang, H. F., Goldstein, S. L., Zhou, X. H., Sun, M., Zheng, J. P., and Cai,
Y.: Evolution of subcontinental lithospheric mantle beneath eastern China:
Re–Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and
Mesozoic basalts, Contrib. Mineral. Petrol., 155, 271–293, 2008.
Zhao, G. C., Sun, M., Wilde, S. A., and Li, S. Z.: Late Archean to
Paleoproterozoic evolution of the North China Craton: key issues revisited,
Precambrian Res., 136, 177–202, 2005.
Zheng, J., Griffin, W. L., O'Reilly, S. Y., Liou, J. G., Zhang, R. Y., and
Fengxiang, L.: Late Mesozoic-Eocene mantle replacement beneath the Eastern
North China craton: evidence from the Paleozoic and Cenozoic peridotite
xenoliths, Int. Geol. Rev., 47, 457–472, 2005.
Zheng, J., Griffin, W. L., O'Reilly, S. Y., Yang, J. S, Li, T. F, Zhang, M.,
Zhang, R. Y., and Liou, J. G.: Mineral chemistry of peridotites from
Paleozoic, Mesozoic and Cenozoic lithosphere: constraints on mantle
evolution beneath eastern China, J. Petrol., 47, 2233–2256, 2006.
Zhu, R. Z., Ni, P., Wang, G. G., Ding, J. Y., and Kang, N.: Temperature and
oxygen state of kimberlite magma from the North China Craton and their
implication for diamond survival, Miner. Deposita, 57, 301–318, 2022.
Short summary
In this work we have applied the elastic geobarometry approach to a Chinese diamond in order to determine the depth of formation of an olivine-bearing diamond. Together with the temperature of residence at which the diamond resided in the mantle, we were able to discover that the diamond was formed at about 190 km depth. Beyond the geological meaning of our results, this work could be a reference paper for future works on Chinese diamonds using elastic geobarometry.
In this work we have applied the elastic geobarometry approach to a Chinese diamond in order to...
