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dc.contributor.author | Ovsyannikov A. | |
dc.contributor.author | Ferlay S. | |
dc.contributor.author | Solovieva S. | |
dc.contributor.author | Antipin I. | |
dc.contributor.author | Konovalov A. | |
dc.contributor.author | Kyritsakas N. | |
dc.contributor.author | Hosseini M. | |
dc.date.accessioned | 2018-09-18T20:35:57Z | |
dc.date.available | 2018-09-18T20:35:57Z | |
dc.date.issued | 2014 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/141548 | |
dc.description.abstract | Combinations of neutral tetrakis meta-pyridyl appended calix[4]arene derivatives in 1,3-A conformation as tectons 3 (tetrakis-meta-pyridyl- tetrathiacalix[4]arene) and 4 (tetrakis-meta- pyridyltetrathiatetramercaptocalix[4]arene) with MX2, behaving as a neutral metallatecton, lead to the formation of 2- and 3-D neutral coordination networks. In all cases, the metal centre adopts a distorted octahedral geometry with the two anions occupying the two apical positions. For compound 3-CdX 2 (X = Cl or Br), 4-CdBr2 and 4-FeCl2 similar porous diamondoid 3D networks, resulting from the tetrakis monodentate behaviour of the organic tectons, are formed. In marked contrast, for 4-CoX2 (X = Cl or Br), only two out of the four pyridyl units take part in the connectivity pattern leading thus to the formation of 2D grid type architectures. This journal is © the Partner Organisations 2014. | |
dc.title | Molecular tectonics: Generation of grid and porous diamondoid coordination networks by calixarene based tectons | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 18 | |
dc.relation.ispartofseries-volume | 16 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 3765 | |
dc.source.id | SCOPUS-2014-16-18-SID84898039178 |