The DOI matches its Crossref record.
Depth of formation of CaSiO 3 -walstromite included in super-deep diamonds
Open accessOverview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Tetrahedrally coordinated carbonate structures match 3-fold ring silicates, such as Ca-walstromite.
“Notably, these structures surprisingly match 3-fold ring silicates, e.g.Ca-walstromite (CaSiO 3 silicate) found as inclusion in diamonds”
From Structures and Crystal Chemistry of Carbonate at Earth's Mantle Conditions (2020) · cites this paper as Anzolini et al., 2016
Citations
Cites
No references could be resolved yet.
Research works printed but not linked: 51
- Angel, 2000, Equations of state, Reviews in Mineralogy and Geochemistry, 41, 35, 10.2138/rmg.2000.41.2 · DOI
- Angel, 2014, EosFit7c and a Fortran module (library) for equation of state calculations, Zeitschrift für Kristallographie, 229, 405, 10.1515/zkri-2013-1711 · DOI
- Angel, 2014, Geobarometry from host-inclusion systems: the role of elastic relaxation, American Mineralogist, 99, 2146, 10.2138/am-2014-5047 · DOI
- Angel, 2015, Diamond thermoelastic properties and implications for determining the pressure of formation of diamond-inclusion systems, Russian Geology and Geophysics, 56, 211, 10.1016/j.rgg.2015.01.014 · DOI
- Angel, 2016, High quality structures at high pressure? Insights from inclusions in diamonds, Zeitschrift für Kristallographie, 231, 467, 10.1515/zkri-2016-1949 · DOI
- Armstrong, 2012, Perovskite phase relations in the system CaO–MgO–TiO2–SiO2 and implications for deep mantle lithologies, Journal of Petrology, 53, 611, 10.1093/petrology/egr073 · DOI
- Barkley, 2011, Structure of walstromite, BaCa2Si3O9, and its relationship to CaSiO3-walstromite and wollastonite-II, American Mineralogist, 96, 797, 10.2138/am.2011.3699 · DOI
- Birch, 1947, Finite elastic strain of cubic crystals, Physical Review, 71, 809, 10.1103/PhysRev.71.809 · DOI
- Blöchl, 1994, Projector augmented-wave method, Physical Review B, 50, 17953, 10.1103/PhysRevB.50.17953 · DOI · Paper page
- Brenker, 2005, Detection of a Ca-rich lithology in the Earth's deep (>300km) convecting mantle, Earth and Planetary Science Letters, 236, 579, 10.1016/j.epsl.2005.05.021 · DOI
- Brenker, 2007, Carbonates from the lower part of transition zone or even the lower mantle, Earth and Planetary Science Letters, 260, 1, 10.1016/j.epsl.2007.02.038 · DOI
- Bulanova, 2010, Mineral inclusions in sublithospheric diamonds from Collier 4 kimberlite pipe, Juina, Brazil: subducted protoliths, carbonated melts and primary kimberlite magmatism, Contributions to Mineralogy and Petrology, 160, 489, 10.1007/s00410-010-0490-6 · DOI
- Day, 2012, A revised diamond-graphite transition curve, American Mineralogist, 97, 52, 10.2138/am.2011.3763 · DOI
- Essene, 1974, High-pressure transformations in CaSiO3, Contributions to Mineralogy and Petrology, 45, 247, 10.1007/BF00383442 · DOI
- Fedortchouk, 2011, An atomic force microscopy study of diamond dissolution features: the effect of H2O and CO2 in the fluid on diamond morphology, American Mineralogist, 96, 1768, 10.2138/am.2011.3828 · DOI
- Gasparik, 1994, Experimental determination of phase relations in the CaSiO3 system from 8 to 15GPa, American Mineralogist, 79, 1219
- Harte, 2010, Diamond formation in the deep mantle: the record of mineral inclusions and their distribution in relation to mantle dehydration zones, Mineralogical Magazine, 74, 189, 10.1180/minmag.2010.074.2.189 · DOI
- Hayman, 2005, Lower mantle diamonds from Rio Soriso (Juina area, Mato Grosso, Brazil), Contributions to Mineralogy and Petrology, 149, 430, 10.1007/s00410-005-0657-8 · DOI
- Holland, 2011, An improved and extended internally consistent thermodynamic dataset for phases of petrological interest, involving a new equation of state for solids, Journal of Metamorphic Geology, 29, 333, 10.1111/j.1525-1314.2010.00923.x · DOI
- Izraeli, 1999, Raman barometry of diamond formation, Earth and Planetary Science Letters, 173, 351, 10.1016/S0012-821X(99)00235-6 · DOI
- Joswig, 1999, New Ca-silicate inclusions in diamonds – tracers from the lower mantle, Earth and Planetary Science Letters, 173, 1, 10.1016/S0012-821X(99)00210-1 · DOI
- Joswig, 2003, The crystal structure of CaSiO3-walstromite, a special isomorph of wollastonite-II, Zeitschrift für Kristallographie, 218, 811, 10.1524/zkri.218.12.811.20547 · DOI
- Kaminsky, 2012, Mineralogy of the lower mantle: a review of ‘super-deep’ mineral inclusions in diamond, Earth Science Reviews, 110, 127, 10.1016/j.earscirev.2011.10.005 · DOI
- Kaminsky, 2001, Superdeep diamonds from the Juina area, Mato Grosso State, Brazil, Contributions to Mineralogy and Petrology, 140, 734, 10.1007/s004100000221 · DOI
- Kanzaki, 1991, Characterization of quenched high pressure phases in CaSiO3 system by XRD and 29Si NMR, Geophysical Research Letters, 18, 463, 10.1029/91GL00463 · DOI
- Kojitani, 2001, Calorimetric study of perovskite solid solutions in the CaSiO3–CaGeO3 system, Physics and Chemistry of Minerals, 28, 413, 10.1007/s002690100166 · DOI
- Kresse, 1996, Efficiency of ab-initio total-energy calculations for metals and semiconductors using a plane-wave basis set, Computational Materials Science, 6, 15, 10.1016/0927-0256(96)00008-0 · DOI
- Kresse, 1996, Efficient iterative schemes for ab-initio total-energy calculations using a plane-wave basis set, Physical Review B, 54, 11169, 10.1103/PhysRevB.54.11169 · DOI · Paper page
- Kresse, 1999, From ultrasoft pseudopotentials to the projector augmented-wave method, Physical Review B, 59, 1758, 10.1103/PhysRevB.59.1758 · DOI · Paper page
- Mao, 1986, Calibration of the ruby pressure gauge to 800kbar under quasi−hydrostatic conditions, Journal of Geophysical Research, 91, 4673, 10.1029/JB091iB05p04673 · DOI
- Merlini, 2013, Single-crystal diffraction at megabar conditions by synchrotron radiation, High Pressure Research, 33, 511, 10.1080/08957959.2013.831088 · DOI · Paper page
- Nasdala, 2003, Spectroscopic 2D-tomography residual pressure and strain around mineral inclusions in diamonds, European Journal of Mineralogy, 15, 931, 10.1127/0935-1221/2003/0015-0931 · DOI
- Nestola, 2011, First crystal-structure determination of olivine in diamond: composition and implications for provenance in the earth's mantle, Earth and Planetary Science Letters, 305, 249, 10.1016/j.epsl.2011.03.007 · DOI
- Nestola, 2012, In situ analysis of garnet inclusion in diamond using single-crystal X-ray diffraction and X-ray micro-tomography, European Journal of Mineralogy, 24, 599, 10.1127/0935-1221/2012/0024-2212 · DOI
- Nestola, 2014, Olivine with diamond-imposed morphology included in diamonds. Syngenesis or protogenesis?, International Geology Review, 56, 1658, 10.1080/00206814.2014.956153 · DOI
- Nestola, 2016, Tetragonal almandine-Pyrope phase, TAPP: finally a name for it, the new mineral jeffbenite, Mineralogical Magazine, 10.1180/minmag.2016.080.059 · DOI
- Pearson, 2014, Hydrous mantle transition zone indicated by ringwoodite included within diamond, Nature, 507, 221, 10.1038/nature13080 · DOI
- Perdew, 1996, Generalized gradient approximation made simple, Physical Review Letters, 77, 3865, 10.1103/PhysRevLett.77.3865 · DOI · Paper page
- Perdew, 2008, Restoring the density-gradient expansion for exchange in solids and surfaces, Physical Review Letters, 100, 136406, 10.1103/PhysRevLett.100.136406 · DOI · Paper page
- Petříček, 2014, Crystallographic computing system JANA2006: general features, Zeitschrift für Kristallographie, 229, 345, 10.1515/zkri-2014-1737 · DOI
- Rebuffi, 2014, MCX: a synchrotron radiation beamline for X−ray diffraction line profile analysis, Zeitschrift für Anorganische und Allgemeine Chemie, 640, 3100, 10.1002/zaac.201400163 · DOI
- Reuss, 1929, Berechnung der fließgrenze von mischkristallen auf grund der plastizitätsbedingung für einkristalle, Journal of Applied Mathematics and Mechanics, 9, 49
- Sobolev, 2000, Fossilized high pressure from the earth's deep interior: the coesite-in-diamond barometer, Proceedings of the National Academy of Sciences of the United States of America, 97, 11875, 10.1073/pnas.220408697 · DOI
- Stachel, 2008, The origin of cratonic diamonds — constraints from mineral inclusions, Ore Geology Reviews, 34, 5, 10.1016/j.oregeorev.2007.05.002 · DOI
- Stachel, 2000, Kankan diamonds (Guinea) II: lower mantle inclusion parageneses, Contributions to Mineralogy and Petrology, 140, 16, 10.1007/s004100000174 · DOI
- Thomson, 2014, Origin of sub-lithospheric diamonds from the Juina-5 kimberlite (Brazil): constraints from carbon isotopes and inclusion compositions, Contributions to Mineralogy and Petrology, 168, 1, 10.1007/s00410-014-1081-8 · DOI
- Thomson, 2016, Trace element composition of silicate inclusions in sub-lithospheric diamonds from the Juina-5 kimberlite: evidence for diamond growth from slab melts, Lithos, 265, 108, 10.1016/j.lithos.2016.08.035 · DOI
- Thomson, 2016, Slab melting as a barrier to deep carbon subduction, Nature, 529, 76, 10.1038/nature16174 · DOI
- Toby, 2001, EXPGUI, a graphical user interface for GSAS, Journal of Applied Crystallography, 34, 210, 10.1107/S0021889801002242 · DOI
- Walter, 2008, Primary carbonatite melt from deeply subducted oceanic crust, Nature, 454, 622, 10.1038/nature07132 · DOI
- Zedgenizov, 2014, Local variations of carbon isotope composition in diamonds from São-Luis (Brazil): evidence for heterogenous carbon reservoir in sublithospheric mantle, Chemical Geology, 363, 114, 10.1016/j.chemgeo.2013.10.033 · DOI
Cited by
Sorted by citations
Structures and Crystal Chemistry of Carbonate at Earth's Mantle Conditions
Merlini, M., Milani, S., & Maurice, J. (2020) · Geophysical Monograph Series · doi:10.1002/9781119508229.ch9 · Cited by 7
“Ca‐walstromite (CaSiO3 silicate) found as inclusion in diamonds, and it has been seen that this phase undergoes polymorphic transition (Anzolini et al., 2016).”
BackgroundSelf-citation
Metadata
- Authors
- Anzolini, C., Angel, R. J., Merlini, M., Derzsi, M., Tokár, K., Milani, S., Krebs, M. Y., Brenker, F. E., Nestola, F., & Harris, J. W.
- Affiliations
- University of Padua (IT)
- University of Milan (IT)
- Slovak Academy of Sciences (SK)
- University of Alberta (CA)
- Goethe University Frankfurt (DE)
- University of Glasgow (GB)
- Corresponding author
- Anzolini, C.
- ORCID
- Venue
- Lithos
- Publisher
- Elsevier BV
- Published
- 2016-11
- Volume
- 265
- Pages
- 138-147
- ISSN
- 0024-4937 (ISSN-L)
- OpenAlex
- W2529320786
- Cited by
- 71
- References
- 0
- Citations by year
- 2026: 1 · 2025: 7 · 2024: 4 · 2023: 5 · 2022: 8 · 2021: 10 · 2020: 10 · 2019: 13 · 2018: 5 · 2017: 6 · 2016: 2
- FWCI
- 7.55
- Type
- journal article
- Language
- en
- Open access
- Licence
- cc-by-nc-nd
- www.elsevier.com/tdm/userlicense/1.0/ (tdm)
- Locations
- Lithos (publishedVersion)
- Padua Research Archive (University of Padova) (submittedVersion, cc-by-nc-nd)
- Funders
- Fondazione Cassa di Risparmio di Padova e Rovigo
- ERC Starting Grant 2012 (307322)
- University of Warsaw (G62-24)
- Diamond Trading Company
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Mineralogy and Gemology Studies
- Keywords
- diamond inclusions, CaSiO3 perovskite, larnite, lower mantle, transition zone, thermodynamic calculation
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review