X-ray and HRTEM study of sursassite: Crystal structure, stacking disorder, and sursassite-pumpellyite intergrowth
X-ray and HRTEM study of sursassite: Crystal structure, stacking disorder, and sursassite-pumpellyite intergrowth
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钠铝锰矿的 X 射线和 HRTEM 研究:晶体结构、堆积无序以及钠铝锰矿-斜方铅矿共生
DOI:
10.1007/bf00309643
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发表时间:
1984
影响因子:
1.4
通讯作者:
M. Pasero
中科院分区:
文献类型:
--
作者:
M. Mellini;S. Merlino;M. Pasero
Sursassite is monoclinic, space groupP21/m, a=8.70,b=5.79,c=9.78 Å, β=108.9°. The crystal structure was determined with X-rays and refined toR=0.065, obtaining Mn2Al3[(OH)3(SiO4)(Si2O7)] as ideal crystal chemical formula. Sursassite, isostructural with macfallite Ca2Mn3[(OH)3(SiO4)(Si2O7)], is closely related to pumpellyite Ca2Al3[(OH)3(SiO4)(Si2O7)]. In fact both sursassite and pumpellyite, apart from the different chemical composition, are built up by common structural layers, which are repeated by different stacking vectors. As a result, faulted stacking sequences are energetically possible.Examination byhigh resolution transmission electron microscopy(HRTEM) shows that frequent (001) pumpellyite-like lamellae are intergrown with thicker (001) sursassite lamellae. Usually, the guest lamellae are a few unit cells thick along [001] and continuous along the (001) plane, although also rare interrupted lamellae are found.