Loading…

New Data on the Isomorphism in Eudialyte-Group Minerals. ХI: Crystal Structure of a Potentially New Mineral—A Case of Complete Substitution of Fe2+with in the Eudialyte-Type Structure

The crystal structure and crystallochemical features of a Fe-deficient zirconium-rich analog of eudialyte from the Lovozero alkaline massif (Kola peninsula) have been investigated. The unit-cell parameters of the mineral are found to be a = 14.198(1) Å, c = 30.380(1) Å, and V = 5303.9(1) Å 3 ; sp. g...

Full description

Saved in:
Bibliographic Details
Published in:Crystallography reports 2022, Vol.67 (2), p.166-171
Main Authors: Rastsvetaeva, R. K., Chukanov, N. V., Pekov, I. V., Varlamov, D. A., Kazheva, O. N.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3
cites cdi_FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3
container_end_page 171
container_issue 2
container_start_page 166
container_title Crystallography reports
container_volume 67
creator Rastsvetaeva, R. K.
Chukanov, N. V.
Pekov, I. V.
Varlamov, D. A.
Kazheva, O. N.
description The crystal structure and crystallochemical features of a Fe-deficient zirconium-rich analog of eudialyte from the Lovozero alkaline massif (Kola peninsula) have been investigated. The unit-cell parameters of the mineral are found to be a = 14.198(1) Å, c = 30.380(1) Å, and V = 5303.9(1) Å 3 ; sp. gr. R 3 m . The crystal structure is refined to the final reliability factor R = 4.2% in the anisotropic approximation of atomic displacements using 3174 reflections with F > 3σ( F ). The crystallochemical formula of the mineral ( Z = 3) is [Na 10.38 (H 3 O,H 2 O) 2.79 Ce 0.45 Sr 0.4 K 0.2 ][Ca 3.9 Mn 1.2 Fe 0.9 ][ VII Na V Zr 0.87 ]Zr 3 [Si 1.48 Ti 0.31 Nb 0.21 ][Si 24 O 72 ](OH) 2.9 (H 2 O) 1.26 (Cl, S) 0.94 (Roman numerals are the coordination numbers (CNs) of cations at the M 2 key site). The regularities of block isomorphism in the vicinity of the M 2 site in the structure of the mineral under study and related eudialyte-group minerals are discussed.
doi_str_mv 10.1134/S1063774522020134
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2652610364</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2652610364</sourcerecordid><originalsourceid>FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3</originalsourceid><addsrcrecordid>eNp1UUtOwzAQjRBIlMIB2FliiVJsx0kcdlVoS6XykVokdpGT2DRVGgfbUZUdh-AKXIJTcAZOgkMrdYFYzWjee_OeZhznHMEBQh65miMYeGFIfIwhhnZy4PSQH2A3oNHzoe0t7Hb4sXOi9QpCSCkiPefznm_ADTMMyAqYJQdTLddS1ctCr0FRgVGTF6xsDXcnSjY1uCsqrlipB-DrY3oNYtVqw0owN6rJTKM4kAIw8CgNr4wVli3oDHaq77f3IYiZ_mXFcl2X3HAwb1JtCtOYwkawwJjjy01hlp19l2gfYdHWfG916hwJm4Sf7WrfeRqPFvGtO3uYTOPhzM1QgIhLqQiDLAox9Yi9i48y6nk4JRQimHIhUMjynIWECgT9yFaYsxTlxM8iIXyee33nYru3VvK14dokK9moylomOPBxgKAXEMtCW1ampNaKi6RWxZqpNkEw6V6U_HmR1eCtRltu9cLVfvP_oh_MkJXJ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2652610364</pqid></control><display><type>article</type><title>New Data on the Isomorphism in Eudialyte-Group Minerals. ХI: Crystal Structure of a Potentially New Mineral—A Case of Complete Substitution of Fe2+with in the Eudialyte-Type Structure</title><source>Springer Link</source><creator>Rastsvetaeva, R. K. ; Chukanov, N. V. ; Pekov, I. V. ; Varlamov, D. A. ; Kazheva, O. N.</creator><creatorcontrib>Rastsvetaeva, R. K. ; Chukanov, N. V. ; Pekov, I. V. ; Varlamov, D. A. ; Kazheva, O. N.</creatorcontrib><description>The crystal structure and crystallochemical features of a Fe-deficient zirconium-rich analog of eudialyte from the Lovozero alkaline massif (Kola peninsula) have been investigated. The unit-cell parameters of the mineral are found to be a = 14.198(1) Å, c = 30.380(1) Å, and V = 5303.9(1) Å 3 ; sp. gr. R 3 m . The crystal structure is refined to the final reliability factor R = 4.2% in the anisotropic approximation of atomic displacements using 3174 reflections with F &gt; 3σ( F ). The crystallochemical formula of the mineral ( Z = 3) is [Na 10.38 (H 3 O,H 2 O) 2.79 Ce 0.45 Sr 0.4 K 0.2 ][Ca 3.9 Mn 1.2 Fe 0.9 ][ VII Na V Zr 0.87 ]Zr 3 [Si 1.48 Ti 0.31 Nb 0.21 ][Si 24 O 72 ](OH) 2.9 (H 2 O) 1.26 (Cl, S) 0.94 (Roman numerals are the coordination numbers (CNs) of cations at the M 2 key site). The regularities of block isomorphism in the vicinity of the M 2 site in the structure of the mineral under study and related eudialyte-group minerals are discussed.</description><identifier>ISSN: 1063-7745</identifier><identifier>EISSN: 1562-689X</identifier><identifier>DOI: 10.1134/S1063774522020134</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Coordination numbers ; Crystal structure ; Crystallography and Scattering Methods ; Iron ; Isomorphism ; Massifs ; Minerals ; Physics ; Physics and Astronomy ; Reliability aspects ; Structure of Inorganic Compounds ; Unit cell ; Zirconium</subject><ispartof>Crystallography reports, 2022, Vol.67 (2), p.166-171</ispartof><rights>Pleiades Publishing, Inc. 2022. ISSN 1063-7745, Crystallography Reports, 2022, Vol. 67, No. 2, pp. 166–171. © Pleiades Publishing, Inc., 2022. Russian Text © The Author(s), 2022, published in Kristallografiya, 2022, Vol. 67, No. 2, pp. 227–232.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3</citedby><cites>FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Rastsvetaeva, R. K.</creatorcontrib><creatorcontrib>Chukanov, N. V.</creatorcontrib><creatorcontrib>Pekov, I. V.</creatorcontrib><creatorcontrib>Varlamov, D. A.</creatorcontrib><creatorcontrib>Kazheva, O. N.</creatorcontrib><title>New Data on the Isomorphism in Eudialyte-Group Minerals. ХI: Crystal Structure of a Potentially New Mineral—A Case of Complete Substitution of Fe2+with in the Eudialyte-Type Structure</title><title>Crystallography reports</title><addtitle>Crystallogr. Rep</addtitle><description>The crystal structure and crystallochemical features of a Fe-deficient zirconium-rich analog of eudialyte from the Lovozero alkaline massif (Kola peninsula) have been investigated. The unit-cell parameters of the mineral are found to be a = 14.198(1) Å, c = 30.380(1) Å, and V = 5303.9(1) Å 3 ; sp. gr. R 3 m . The crystal structure is refined to the final reliability factor R = 4.2% in the anisotropic approximation of atomic displacements using 3174 reflections with F &gt; 3σ( F ). The crystallochemical formula of the mineral ( Z = 3) is [Na 10.38 (H 3 O,H 2 O) 2.79 Ce 0.45 Sr 0.4 K 0.2 ][Ca 3.9 Mn 1.2 Fe 0.9 ][ VII Na V Zr 0.87 ]Zr 3 [Si 1.48 Ti 0.31 Nb 0.21 ][Si 24 O 72 ](OH) 2.9 (H 2 O) 1.26 (Cl, S) 0.94 (Roman numerals are the coordination numbers (CNs) of cations at the M 2 key site). The regularities of block isomorphism in the vicinity of the M 2 site in the structure of the mineral under study and related eudialyte-group minerals are discussed.</description><subject>Coordination numbers</subject><subject>Crystal structure</subject><subject>Crystallography and Scattering Methods</subject><subject>Iron</subject><subject>Isomorphism</subject><subject>Massifs</subject><subject>Minerals</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Reliability aspects</subject><subject>Structure of Inorganic Compounds</subject><subject>Unit cell</subject><subject>Zirconium</subject><issn>1063-7745</issn><issn>1562-689X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1UUtOwzAQjRBIlMIB2FliiVJsx0kcdlVoS6XykVokdpGT2DRVGgfbUZUdh-AKXIJTcAZOgkMrdYFYzWjee_OeZhznHMEBQh65miMYeGFIfIwhhnZy4PSQH2A3oNHzoe0t7Hb4sXOi9QpCSCkiPefznm_ADTMMyAqYJQdTLddS1ctCr0FRgVGTF6xsDXcnSjY1uCsqrlipB-DrY3oNYtVqw0owN6rJTKM4kAIw8CgNr4wVli3oDHaq77f3IYiZ_mXFcl2X3HAwb1JtCtOYwkawwJjjy01hlp19l2gfYdHWfG916hwJm4Sf7WrfeRqPFvGtO3uYTOPhzM1QgIhLqQiDLAox9Yi9i48y6nk4JRQimHIhUMjynIWECgT9yFaYsxTlxM8iIXyee33nYru3VvK14dokK9moylomOPBxgKAXEMtCW1ampNaKi6RWxZqpNkEw6V6U_HmR1eCtRltu9cLVfvP_oh_MkJXJ</recordid><startdate>2022</startdate><enddate>2022</enddate><creator>Rastsvetaeva, R. K.</creator><creator>Chukanov, N. V.</creator><creator>Pekov, I. V.</creator><creator>Varlamov, D. A.</creator><creator>Kazheva, O. N.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>2022</creationdate><title>New Data on the Isomorphism in Eudialyte-Group Minerals. ХI: Crystal Structure of a Potentially New Mineral—A Case of Complete Substitution of Fe2+with in the Eudialyte-Type Structure</title><author>Rastsvetaeva, R. K. ; Chukanov, N. V. ; Pekov, I. V. ; Varlamov, D. A. ; Kazheva, O. N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Coordination numbers</topic><topic>Crystal structure</topic><topic>Crystallography and Scattering Methods</topic><topic>Iron</topic><topic>Isomorphism</topic><topic>Massifs</topic><topic>Minerals</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Reliability aspects</topic><topic>Structure of Inorganic Compounds</topic><topic>Unit cell</topic><topic>Zirconium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rastsvetaeva, R. K.</creatorcontrib><creatorcontrib>Chukanov, N. V.</creatorcontrib><creatorcontrib>Pekov, I. V.</creatorcontrib><creatorcontrib>Varlamov, D. A.</creatorcontrib><creatorcontrib>Kazheva, O. N.</creatorcontrib><collection>CrossRef</collection><jtitle>Crystallography reports</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rastsvetaeva, R. K.</au><au>Chukanov, N. V.</au><au>Pekov, I. V.</au><au>Varlamov, D. A.</au><au>Kazheva, O. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New Data on the Isomorphism in Eudialyte-Group Minerals. ХI: Crystal Structure of a Potentially New Mineral—A Case of Complete Substitution of Fe2+with in the Eudialyte-Type Structure</atitle><jtitle>Crystallography reports</jtitle><stitle>Crystallogr. Rep</stitle><date>2022</date><risdate>2022</risdate><volume>67</volume><issue>2</issue><spage>166</spage><epage>171</epage><pages>166-171</pages><issn>1063-7745</issn><eissn>1562-689X</eissn><abstract>The crystal structure and crystallochemical features of a Fe-deficient zirconium-rich analog of eudialyte from the Lovozero alkaline massif (Kola peninsula) have been investigated. The unit-cell parameters of the mineral are found to be a = 14.198(1) Å, c = 30.380(1) Å, and V = 5303.9(1) Å 3 ; sp. gr. R 3 m . The crystal structure is refined to the final reliability factor R = 4.2% in the anisotropic approximation of atomic displacements using 3174 reflections with F &gt; 3σ( F ). The crystallochemical formula of the mineral ( Z = 3) is [Na 10.38 (H 3 O,H 2 O) 2.79 Ce 0.45 Sr 0.4 K 0.2 ][Ca 3.9 Mn 1.2 Fe 0.9 ][ VII Na V Zr 0.87 ]Zr 3 [Si 1.48 Ti 0.31 Nb 0.21 ][Si 24 O 72 ](OH) 2.9 (H 2 O) 1.26 (Cl, S) 0.94 (Roman numerals are the coordination numbers (CNs) of cations at the M 2 key site). The regularities of block isomorphism in the vicinity of the M 2 site in the structure of the mineral under study and related eudialyte-group minerals are discussed.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1063774522020134</doi><tpages>6</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1063-7745
ispartof Crystallography reports, 2022, Vol.67 (2), p.166-171
issn 1063-7745
1562-689X
language eng
recordid cdi_proquest_journals_2652610364
source Springer Link
subjects Coordination numbers
Crystal structure
Crystallography and Scattering Methods
Iron
Isomorphism
Massifs
Minerals
Physics
Physics and Astronomy
Reliability aspects
Structure of Inorganic Compounds
Unit cell
Zirconium
title New Data on the Isomorphism in Eudialyte-Group Minerals. ХI: Crystal Structure of a Potentially New Mineral—A Case of Complete Substitution of Fe2+with in the Eudialyte-Type Structure
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-23T18%3A14%3A34IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=New%20Data%20on%20the%20Isomorphism%20in%20Eudialyte-Group%20Minerals.%20%D0%A5I:%20Crystal%20Structure%20of%20a%20Potentially%20New%20Mineral%E2%80%94A%20Case%20of%20Complete%20Substitution%20of%20Fe2+with%20in%20the%20Eudialyte-Type%20Structure&rft.jtitle=Crystallography%20reports&rft.au=Rastsvetaeva,%20R.%20K.&rft.date=2022&rft.volume=67&rft.issue=2&rft.spage=166&rft.epage=171&rft.pages=166-171&rft.issn=1063-7745&rft.eissn=1562-689X&rft_id=info:doi/10.1134/S1063774522020134&rft_dat=%3Cproquest_cross%3E2652610364%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c1614-88f76c97283413451c8332b48010beff17adda748f10597480dab1d45c9ff5ed3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2652610364&rft_id=info:pmid/&rfr_iscdi=true