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Transition of Metastable Pyrrhotites to a Stable Phase State

https://doi.org/10.1134/s0020168520090137
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12/12 checkable references clean · checked 2026-07-23

Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a retraction, withdrawal, or removal notice.

11 without a DOI — not checked. A reference deposited without a DOI is never matched by title or guessed at; it stays outside the checked set, and this line discloses that.

The 12 checked references that resolve
resolves10.1021/cr0503658
Chemistry of Iron Sulfides
resolves10.2138/am.2006.2347
High-pressure study of FeS, between 20 and 120 GPa, using synchrotron X-ray powder diffraction
resolves10.1111/maps.12145
Raman spectroscopic properties and Raman identification of CaS‐MgS‐MnS‐FeS‐Cr<sub>2</sub>FeS<sub>4</sub> sulfides in meteorites and reduced sulfur‐rich systems
resolves10.2138/am.2006.1999
Inversion twinning in troilite
resolves10.1080/01411590500185542
A review on the mineral chemistry of the non-stoichiometric iron sulphide, Fe<sub>1−</sub><b><i><sub>x</sub></i></b>S (0 ≤ <b><i>x</i></b> ≤ 0.125): polymorphs, phase relations and transitions, electronic and magnetic structures
resolves10.1134/S003602361503002X
Thermal and thermomagnetic properties of pyrrhotites
resolves10.2138/am.2012.3887
Redetermination of the structure of 5C pyrrhotite at low temperature and at room temperature
resolves10.1126/science.168.3934.964
Pyrrhotites: Stoichiometric Compounds with Composition Fe <sub> <i>n</i> -1 </sub> S <sub> <i>n</i> </sub> ( <i>n</i> ≥ 8)
resolves10.2113/gsecongeo.57.1.72
Equilibrium relations between pyrrhotite and pyrite from 325 degrees to 743 degrees C
resolves10.2113/gsecongeo.54.4.533
Pyrite stability relations in the Fe-S system
resolves10.3891/acta.chem.scand.06-1452
On the Phase Relations of Synthetic and Natural Pyrrhotites (Fe(1-x)S).
resolves10.2113/gsecongeo.70.4.824
Crystallography and stability of pyrrhotites
The 11 references without a DOI — listed, not checked
no DOI — not checkedNovikov, G.V., Egorov, V.K., and Sokolov, Yu.A., Pirrotiny: kristallicheskaya i magnitnaya struktura (Pyrrhotites: Crystal and Magnetic Structures), Moscow: Nauka, 1988.
no DOI — not checkedDeer, W.A., Howie, R.A., and Zussman, J., Rock-Forming Minerals, New York: Wiley, 1962–1963, vol. 5.
no DOI — not checkedWard, J., The structure and properties of some iron sulphides, Rev. Pure Appl. Chem., 1970, vol. 20, pp. 175–206.
no DOI — not checkedFleet, M.E., Structural aspects of the marcasite–pyrite transformation, Can. Mineral., 1970, vol. 10, pp. 225–231.
no DOI — not checkedGait, R.I. and Dumka, D., Morphology of pyrite from the Nanisivik Mine, Baffin Island, Northwest Territories, Can. Mineral., 1986, vol. 24, pp. 685–688.
no DOI — not checkedOnufrienock, V.V. and Zvegintzev, A.G., Temperature magnetic hysteresis of pirrotines, Geomagn. Aeron., 1981, vol. 21, pp. 575–577.
no DOI — not checkedOnufrienok, V.V. and Zvegintsev, A.G., Magnetic properties and crystal structure of iron sulfides in the composition range FeS–FeS1.18, Izv. Akad. Nauk SSSR,Neorg. Mater., 1982, vol. 18, no. 3, pp. 366–371.
no DOI — not checkedSelivanov, E.N. and Gulyaeva, R.I., Thermal expansion and phase transformations of natural pyrrhotite, Russ. J. Inorg. Mater., 2008, vol. 44, pp. 506–511.
no DOI — not checkedZvegintsev, A.G. and Onufrienok, V.V., Magnetic properties of pyrrhotites that resulted from pyrite decomposition, Geomagn. Aeron., 1981, vol. 21, no. 4, pp. 763–765.
no DOI — not checkedFleet, M.E., On the lattice parameters and superstructures of pyrrhotites, Am. Mineral., 1968, vol. 53, pp. 1346–1351.
no DOI — not checkedArnold, R.G., The pyrrhotite–pyrite relationship, Ann. Rep. Dir. Geophys. Lab., 1956, vol. 55, pp. 177–183.
What this badge says. CiteStamped means the CHECKABLE references of this work were clean at the dated check: each resolved to a known work in a public registry, and none carried a retraction notice at that time. It says nothing about the quality, findings, or importance of the work itself, and nothing about references deposited without a DOI.

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