2007
DOI: 10.1016/j.tsf.2006.12.100
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Structural aspects of adamantine like multinary chalcogenides

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Cited by 156 publications
(88 citation statements)
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“…4(b)], due to the coordination increase of the metal cations with respect to sulfur anions from fourfold to sixfold. Given that the kesterite phase is structurally related to the sphalerite-and chalcopyrite-type structures, 10 the pressure-induced transition towards a RS-type phase is consistent with the general trend of the latter structures upon compression. 46,47 As for the observation of Raman signal in the stability range of the Raman-inactive NaCl-type phase [inset in Fig.…”
supporting
confidence: 73%
See 1 more Smart Citation
“…4(b)], due to the coordination increase of the metal cations with respect to sulfur anions from fourfold to sixfold. Given that the kesterite phase is structurally related to the sphalerite-and chalcopyrite-type structures, 10 the pressure-induced transition towards a RS-type phase is consistent with the general trend of the latter structures upon compression. 46,47 As for the observation of Raman signal in the stability range of the Raman-inactive NaCl-type phase [inset in Fig.…”
supporting
confidence: 73%
“…8,9 This phase is structurally derived from the sphalerite-type structure by a doubling of the respective c-axis, resulting from alternating cationic (Cu/Sn or Cu/Zn) layers separated by sulfur anions. 10 Consequently, all of the cations are tetrahedrally coordinated with respect to the anions. Even though the KS phase represents an ordered cationic arrangement, i.e., each cation occupies a unique Wyckoff site, cationic disorder is quite common in this material.…”
mentioning
confidence: 99%
“…CZTS crystallizes with the kesterite/stannite structure, I-4/I42m space group which is of the adamantine family [14]. Its unit cell parameters are a: 5.435 Å and c: 10.843 Å [15].…”
Section: Xrd Analysismentioning
confidence: 99%
“…The energy difference per atom with respect to the stannite structure (I42m) is only of few meV per atom, 3,4,9 proving that kesterite and stannite phases can coexist in experimental samples, and explaining the reported disordered structures. 10 Similarly to chalcopyrites CIGS, quaternary kesterite and stannite CZTS are obtained from the zincblende structure by replacing the Zn cations in such a way that each anion (Se or S) is coordinated by one Zn, one Sn and two Cu atoms. The existence of three distinct cations results in three different cationanion bond lengths, which induce a displacement of the anion from its ideal zincblende site.…”
Section: 8mentioning
confidence: 99%