<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE root>
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Priroda</journal-id><journal-title-group><journal-title xml:lang="en">Priroda</journal-title><trans-title-group xml:lang="ru"><trans-title>Природа</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0032-874X</issn><publisher><publisher-name xml:lang="en">Akademizdatcenter Nauka</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">627696</article-id><article-id pub-id-type="doi">10.7868/S0032874X22090058</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Born by Volcano: New Mineral Khrenovite</article-title><trans-title-group xml:lang="ru"><trans-title>Рожденный вулканом: новый минерал хреновит</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Rastsvetaeva</surname><given-names>R. K</given-names></name><name xml:lang="ru"><surname>Расцветаева</surname><given-names>Р. К</given-names></name></name-alternatives><email>rast.crys@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Shubnikov Institute of Crystallography, Federal Scientific Research Centre “Crystallography and Photonics”, Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Институт кристаллографии имени А.В.Шубникова Федерального научно-исследовательского центра «Кристаллография и фотоника» РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2022-09-30" publication-format="electronic"><day>30</day><month>09</month><year>2022</year></pub-date><issue>9</issue><issue-title xml:lang="en">NO9 (2022)</issue-title><issue-title xml:lang="ru">№9 (2022)</issue-title><fpage>40</fpage><lpage>41</lpage><history><date date-type="received" iso-8601-date="2024-03-01"><day>01</day><month>03</month><year>2024</year></date></history><permissions><copyright-statement xml:lang="ru">Copyright ©; 2022, Издательство «Наука»</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Издательство «Наука»</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/0032-874X/article/view/627696">https://journals.eco-vector.com/0032-874X/article/view/627696</self-uri><abstract xml:lang="en"><p>List of minerals recognized by the International Mineralogical Association contents about 6000 mineral species and each year it is upsized by 50–60 new minerals. Russian scientists are also among the discoverers of these new species. The most perspective for the new mineral discovery on the Russian territory are the Khibiny Mountains and Lovozero Massif of the Kola Peninsula as well as Kamchatka volcanic region. This article reports on recent discovery of khrenovite Na3Fe23+(AsO4)3, a new arsenate member of alluaudite group from fumarole of Tolbachik volcano.</p></abstract><trans-abstract xml:lang="ru"><p>Кадастр минеральных видов насчитывает около 6 тыс. представителей, и каждый год он пополняется в среднем на 50–60 новых минералов. Среди их открывателей — и российские ученые. Наиболее перспективны для открытия новых минералов на территории России — Хибинский и Ловозерский массивы Кольского п-ова, а также Камчатские вулканические регионы. В данной статье рассказывается о недавнем открытии нового минерала хреновита Na3Fe23+(AsO4)3 — арсенатного представителя группы аллюодита из фумаролы Толбачинского вулкана.</p></trans-abstract><kwd-group xml:lang="en"><kwd>arsenate</kwd><kwd>khrenovite</kwd><kwd>new mineral</kwd><kwd>alluaudite group</kwd><kwd>crystal structure</kwd><kwd>fumarole</kwd><kwd>Tolbachik volcano</kwd><kwd>Kamchatka</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>арсенаты</kwd><kwd>хреновит</kwd><kwd>новый минерал</kwd><kwd>группа аллюодита</kwd><kwd>кристаллическая структура</kwd><kwd>фумарола</kwd><kwd>Толбачик</kwd><kwd>Камчатка</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Pekov I.V., Koshlyakova N.N., Belakovskiy D.I. et al. New arsenate minerals from the Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. XVIII. Khrenovite, Na3Fe2</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>3+(AsO4)3, the sodium-richest alluaudite-supergroup member. Mineralogical Magazine. 2022; 86: 1–17. DOI:10.1180/mgm.2022.64.</mixed-citation></ref><ref id="B3"><label>3.</label><mixed-citation>Pekov I.V., Zubkova N.V., Yapaskurt V.O. et al. New arsenate minerals from the Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. I. Yurmarinite, Na7(Fe3+,Mg,Cu)4(AsO4)6. Mineralogical Magazine. 2014; 78: 905–917.</mixed-citation></ref><ref id="B4"><label>4.</label><mixed-citation>Pekov I.V., Koshlyakova N.N., Zubkova N.V. et al. Fumarolic arsenates — a special type of arsenic mineralization. European Journal of Mineralogy. 2018; 30: 305–322.</mixed-citation></ref><ref id="B5"><label>5.</label><mixed-citation>Shchipalkina N.V., Pekov I.V., Koshlyakova N.N. et al. Unusual silicate mineralization in fumarolic sublimates of the Tolbachik volcano, Kamchatka, Russia — Part 1: Neso-, cyclo-, ino- and phyllosilicates. European Journal of Mineralogy. 2020; 32: 101–119.</mixed-citation></ref><ref id="B6"><label>6.</label><mixed-citation>Moore P.B. Crystal chemistry of the alluaudite structure type: contribution to the paragenesis of pegmatite phosphate giant crystals. Amer. Miner. 1971; 56: 1955–1975.</mixed-citation></ref><ref id="B7"><label>7.</label><mixed-citation>Tait K.T., Hawthorne F.C., Halden N.M. Alluaudite — group phosphate and arsenate vinerals. Canad. Miner. 2021; 59(1): 243–263.</mixed-citation></ref><ref id="B8"><label>8.</label><mixed-citation>Khorari S., Rulmont A., Tarte P. Alluaudite-like structure of the arsenate Na3In2(AsO4)3. Journal of Solid State Chemistry. 1997; 134(1): 31–37.</mixed-citation></ref></ref-list></back></article>
