Ziminaite, Fe3+VO4, a new howardevansite-group mineral from the Bezymyannyi volcano, Kamchatka, Russia
The new mineral ziminaite, ideally Fe 3+ VO 4 , was found in fumarole sublimates at the Bezymyannyi volcano, Kamchatka, Russia. Ziminaite occurs as lamellar, tabular or flattened prismatic crystals up to 10 × 30 × 50 μm typically epitaxially overgrowing koksharovite, and as aggregates (up to 0.15 mm...
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| description | The new mineral ziminaite, ideally Fe
3+
VO
4
, was found in fumarole sublimates at the Bezymyannyi volcano, Kamchatka, Russia. Ziminaite occurs as lamellar, tabular or flattened prismatic crystals up to 10 × 30 × 50 μm typically epitaxially overgrowing koksharovite, and as aggregates (up to 0.15 mm) associated with bannermanite in cavities in volcanic scoria. The mineral is translucent, yellowish-brown with an adamantine luster. The calculated density is 3.45 g cm
− 3
. In reflected light, ziminaite is light grey. Bireflectance is weak, internal reflections are deep yellow. The reflectance values [
R
max
–R
min
, % (λ, nm)] are: 17.7–16.3 (470), 15.7–14.1 (546), 15.1–13.8 (589), 14.7–13.6 (650). Chemical composition (wt%) is: MgO 2.20, CaO 0.01, Al
2
O
3
7.81, Fe
2
O
3
27.18, TiO
2
4.50, SiO
2
0.26, P
2
O
5
0.09, V
2
O
5
57.01, total 99.06. The empirical formula, based on 24 O atoms, is: (Fe
3 +
3.29
Al
1.48
Ti
0.54
Mg
0.53
)
Σ5.84
(V
6.05
Si
0.04
P
0.01
)
Σ6.10
O
24
(Z = 1). Ziminaite is triclinic,
P
1
¯
,
a
8.012(4),
b
9.345(5),
c
6.678(3) Å, α 106.992(10), β 101.547(8), γ 96.594(11)º,
V
460.4(4) Å
3
, Z = 6. The strongest reflections of the powder X-ray diffraction pattern [
d
,Å(
I
)(
hkl
)] are: 3.751(17)(1–21, 12 − 1), 3.539(86)(120), 3.270(67)(01–2), 3.209(100)(2–20), 3.090(20)(2–11, 002), 3.041(18)(03 − 1, 02–2), 2.934(14)(12 − 2, 030) and 1.665(24)(023, 12 − 4). The crystal structure, solved from single-crystal data (
R
1
= 0.085), is based upon heteropolyhedral framework built by VO
4
tetrahedra and Fe
3+
-centred octahedra and five-fold polyhedra. Ziminaite belongs to the howardevansite group being its first member without species-defining uni- or divalent cations and with all large cation sites vacant. The mineral is named after the Zimina volcano situated near the discovery locality. |
| doi_str_mv | 10.1007/s00710-017-0550-y |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1972122373</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1972122373</sourcerecordid><originalsourceid>FETCH-LOGICAL-c246t-d209a396e0f5d2e5f15095898aaf1d9f7cd05df63a75ef70af4849723fd002943</originalsourceid><addsrcrecordid>eNp1kLFOwzAQhi0EEqXwAGyWGKnhHMeJM0JFAVGpEgIGFuuU2G1KkxQ7aRWeHqMwsLDcDff9_0kfIeccrjhAeu3D4MCApwykBNYfkBGPhWKcJ-qQjCAT4ZqCOiYn3q8BQEnFR8S-l1VZY9maCZ0Zcfm2iCcUaW32dNXs0RVmh7UPZ7Z0TbelATYON9S6pqLtytBb89VXPdZ1X9Jds8mxbib0Cat8he0HTuhz532Jp-TI4sabs989Jq-zu5fpA5sv7h-nN3OWR3HSsiKCDEWWGLCyiIy0XEImVaYQLS8ym-YFyMImAlNpbApoYxVnaSRsARBlsRiTi6F365rPzvhWr5vO1eGl5oHjUSRSESg-ULlrvHfG6q0rK3S95qB_dOpBpw469Y9O3YdMNGR8YOulcX-a_w19A54Yd-I</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1972122373</pqid></control><display><type>article</type><title>Ziminaite, Fe3+VO4, a new howardevansite-group mineral from the Bezymyannyi volcano, Kamchatka, Russia</title><source>SpringerLink Journals - AutoHoldings</source><creator>Pekov, Igor V. ; Siidra, Oleg I. ; Yapaskurt, Vasiliy O. ; Polekhovsky, Yury S. ; Kartashov, Pavel M.</creator><creatorcontrib>Pekov, Igor V. ; Siidra, Oleg I. ; Yapaskurt, Vasiliy O. ; Polekhovsky, Yury S. ; Kartashov, Pavel M.</creatorcontrib><description>The new mineral ziminaite, ideally Fe
3+
VO
4
, was found in fumarole sublimates at the Bezymyannyi volcano, Kamchatka, Russia. Ziminaite occurs as lamellar, tabular or flattened prismatic crystals up to 10 × 30 × 50 μm typically epitaxially overgrowing koksharovite, and as aggregates (up to 0.15 mm) associated with bannermanite in cavities in volcanic scoria. The mineral is translucent, yellowish-brown with an adamantine luster. The calculated density is 3.45 g cm
− 3
. In reflected light, ziminaite is light grey. Bireflectance is weak, internal reflections are deep yellow. The reflectance values [
R
max
–R
min
, % (λ, nm)] are: 17.7–16.3 (470), 15.7–14.1 (546), 15.1–13.8 (589), 14.7–13.6 (650). Chemical composition (wt%) is: MgO 2.20, CaO 0.01, Al
2
O
3
7.81, Fe
2
O
3
27.18, TiO
2
4.50, SiO
2
0.26, P
2
O
5
0.09, V
2
O
5
57.01, total 99.06. The empirical formula, based on 24 O atoms, is: (Fe
3 +
3.29
Al
1.48
Ti
0.54
Mg
0.53
)
Σ5.84
(V
6.05
Si
0.04
P
0.01
)
Σ6.10
O
24
(Z = 1). Ziminaite is triclinic,
P
1
¯
,
a
8.012(4),
b
9.345(5),
c
6.678(3) Å, α 106.992(10), β 101.547(8), γ 96.594(11)º,
V
460.4(4) Å
3
, Z = 6. The strongest reflections of the powder X-ray diffraction pattern [
d
,Å(
I
)(
hkl
)] are: 3.751(17)(1–21, 12 − 1), 3.539(86)(120), 3.270(67)(01–2), 3.209(100)(2–20), 3.090(20)(2–11, 002), 3.041(18)(03 − 1, 02–2), 2.934(14)(12 − 2, 030) and 1.665(24)(023, 12 − 4). The crystal structure, solved from single-crystal data (
R
1
= 0.085), is based upon heteropolyhedral framework built by VO
4
tetrahedra and Fe
3+
-centred octahedra and five-fold polyhedra. Ziminaite belongs to the howardevansite group being its first member without species-defining uni- or divalent cations and with all large cation sites vacant. The mineral is named after the Zimina volcano situated near the discovery locality.</description><identifier>ISSN: 0930-0708</identifier><identifier>EISSN: 1438-1168</identifier><identifier>DOI: 10.1007/s00710-017-0550-y</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Aluminum oxide ; Cations ; Composition ; Crystal structure ; Crystals ; Diffraction ; Diffraction patterns ; Divalent cations ; Earth and Environmental Science ; Earth Sciences ; Frameworks ; Geochemistry ; Inorganic Chemistry ; Iron ; Luster ; Mineralogy ; Original Paper ; Polyhedra ; Reflectance ; Silicon dioxide ; Single crystals ; Titanium dioxide ; Vanadium pentoxide ; Volcanic activity ; Volcanoes ; X ray powder diffraction ; X-ray diffraction ; X-rays</subject><ispartof>Mineralogy and petrology, 2018-06, Vol.112 (3), p.371-379</ispartof><rights>Springer-Verlag GmbH Austria, part of Springer Nature 2017</rights><rights>Mineralogy and Petrology is a copyright of Springer, (2017). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c246t-d209a396e0f5d2e5f15095898aaf1d9f7cd05df63a75ef70af4849723fd002943</citedby><cites>FETCH-LOGICAL-c246t-d209a396e0f5d2e5f15095898aaf1d9f7cd05df63a75ef70af4849723fd002943</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00710-017-0550-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00710-017-0550-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,778,782,27907,27908,41471,42540,51302</link.rule.ids></links><search><creatorcontrib>Pekov, Igor V.</creatorcontrib><creatorcontrib>Siidra, Oleg I.</creatorcontrib><creatorcontrib>Yapaskurt, Vasiliy O.</creatorcontrib><creatorcontrib>Polekhovsky, Yury S.</creatorcontrib><creatorcontrib>Kartashov, Pavel M.</creatorcontrib><title>Ziminaite, Fe3+VO4, a new howardevansite-group mineral from the Bezymyannyi volcano, Kamchatka, Russia</title><title>Mineralogy and petrology</title><addtitle>Miner Petrol</addtitle><description>The new mineral ziminaite, ideally Fe
3+
VO
4
, was found in fumarole sublimates at the Bezymyannyi volcano, Kamchatka, Russia. Ziminaite occurs as lamellar, tabular or flattened prismatic crystals up to 10 × 30 × 50 μm typically epitaxially overgrowing koksharovite, and as aggregates (up to 0.15 mm) associated with bannermanite in cavities in volcanic scoria. The mineral is translucent, yellowish-brown with an adamantine luster. The calculated density is 3.45 g cm
− 3
. In reflected light, ziminaite is light grey. Bireflectance is weak, internal reflections are deep yellow. The reflectance values [
R
max
–R
min
, % (λ, nm)] are: 17.7–16.3 (470), 15.7–14.1 (546), 15.1–13.8 (589), 14.7–13.6 (650). Chemical composition (wt%) is: MgO 2.20, CaO 0.01, Al
2
O
3
7.81, Fe
2
O
3
27.18, TiO
2
4.50, SiO
2
0.26, P
2
O
5
0.09, V
2
O
5
57.01, total 99.06. The empirical formula, based on 24 O atoms, is: (Fe
3 +
3.29
Al
1.48
Ti
0.54
Mg
0.53
)
Σ5.84
(V
6.05
Si
0.04
P
0.01
)
Σ6.10
O
24
(Z = 1). Ziminaite is triclinic,
P
1
¯
,
a
8.012(4),
b
9.345(5),
c
6.678(3) Å, α 106.992(10), β 101.547(8), γ 96.594(11)º,
V
460.4(4) Å
3
, Z = 6. The strongest reflections of the powder X-ray diffraction pattern [
d
,Å(
I
)(
hkl
)] are: 3.751(17)(1–21, 12 − 1), 3.539(86)(120), 3.270(67)(01–2), 3.209(100)(2–20), 3.090(20)(2–11, 002), 3.041(18)(03 − 1, 02–2), 2.934(14)(12 − 2, 030) and 1.665(24)(023, 12 − 4). The crystal structure, solved from single-crystal data (
R
1
= 0.085), is based upon heteropolyhedral framework built by VO
4
tetrahedra and Fe
3+
-centred octahedra and five-fold polyhedra. Ziminaite belongs to the howardevansite group being its first member without species-defining uni- or divalent cations and with all large cation sites vacant. The mineral is named after the Zimina volcano situated near the discovery locality.</description><subject>Aluminum oxide</subject><subject>Cations</subject><subject>Composition</subject><subject>Crystal structure</subject><subject>Crystals</subject><subject>Diffraction</subject><subject>Diffraction patterns</subject><subject>Divalent cations</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Frameworks</subject><subject>Geochemistry</subject><subject>Inorganic Chemistry</subject><subject>Iron</subject><subject>Luster</subject><subject>Mineralogy</subject><subject>Original Paper</subject><subject>Polyhedra</subject><subject>Reflectance</subject><subject>Silicon dioxide</subject><subject>Single crystals</subject><subject>Titanium dioxide</subject><subject>Vanadium pentoxide</subject><subject>Volcanic activity</subject><subject>Volcanoes</subject><subject>X ray powder diffraction</subject><subject>X-ray diffraction</subject><subject>X-rays</subject><issn>0930-0708</issn><issn>1438-1168</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp1kLFOwzAQhi0EEqXwAGyWGKnhHMeJM0JFAVGpEgIGFuuU2G1KkxQ7aRWeHqMwsLDcDff9_0kfIeccrjhAeu3D4MCApwykBNYfkBGPhWKcJ-qQjCAT4ZqCOiYn3q8BQEnFR8S-l1VZY9maCZ0Zcfm2iCcUaW32dNXs0RVmh7UPZ7Z0TbelATYON9S6pqLtytBb89VXPdZ1X9Jds8mxbib0Cat8he0HTuhz532Jp-TI4sabs989Jq-zu5fpA5sv7h-nN3OWR3HSsiKCDEWWGLCyiIy0XEImVaYQLS8ym-YFyMImAlNpbApoYxVnaSRsARBlsRiTi6F365rPzvhWr5vO1eGl5oHjUSRSESg-ULlrvHfG6q0rK3S95qB_dOpBpw469Y9O3YdMNGR8YOulcX-a_w19A54Yd-I</recordid><startdate>20180601</startdate><enddate>20180601</enddate><creator>Pekov, Igor V.</creator><creator>Siidra, Oleg I.</creator><creator>Yapaskurt, Vasiliy O.</creator><creator>Polekhovsky, Yury S.</creator><creator>Kartashov, Pavel M.</creator><general>Springer Vienna</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20180601</creationdate><title>Ziminaite, Fe3+VO4, a new howardevansite-group mineral from the Bezymyannyi volcano, Kamchatka, Russia</title><author>Pekov, Igor V. ; Siidra, Oleg I. ; Yapaskurt, Vasiliy O. ; Polekhovsky, Yury S. ; Kartashov, Pavel M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c246t-d209a396e0f5d2e5f15095898aaf1d9f7cd05df63a75ef70af4849723fd002943</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Aluminum oxide</topic><topic>Cations</topic><topic>Composition</topic><topic>Crystal structure</topic><topic>Crystals</topic><topic>Diffraction</topic><topic>Diffraction patterns</topic><topic>Divalent cations</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Frameworks</topic><topic>Geochemistry</topic><topic>Inorganic Chemistry</topic><topic>Iron</topic><topic>Luster</topic><topic>Mineralogy</topic><topic>Original Paper</topic><topic>Polyhedra</topic><topic>Reflectance</topic><topic>Silicon dioxide</topic><topic>Single crystals</topic><topic>Titanium dioxide</topic><topic>Vanadium pentoxide</topic><topic>Volcanic activity</topic><topic>Volcanoes</topic><topic>X ray powder diffraction</topic><topic>X-ray diffraction</topic><topic>X-rays</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pekov, Igor V.</creatorcontrib><creatorcontrib>Siidra, Oleg I.</creatorcontrib><creatorcontrib>Yapaskurt, Vasiliy O.</creatorcontrib><creatorcontrib>Polekhovsky, Yury S.</creatorcontrib><creatorcontrib>Kartashov, Pavel M.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Mineralogy and petrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pekov, Igor V.</au><au>Siidra, Oleg I.</au><au>Yapaskurt, Vasiliy O.</au><au>Polekhovsky, Yury S.</au><au>Kartashov, Pavel M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Ziminaite, Fe3+VO4, a new howardevansite-group mineral from the Bezymyannyi volcano, Kamchatka, Russia</atitle><jtitle>Mineralogy and petrology</jtitle><stitle>Miner Petrol</stitle><date>2018-06-01</date><risdate>2018</risdate><volume>112</volume><issue>3</issue><spage>371</spage><epage>379</epage><pages>371-379</pages><issn>0930-0708</issn><eissn>1438-1168</eissn><abstract>The new mineral ziminaite, ideally Fe
3+
VO
4
, was found in fumarole sublimates at the Bezymyannyi volcano, Kamchatka, Russia. Ziminaite occurs as lamellar, tabular or flattened prismatic crystals up to 10 × 30 × 50 μm typically epitaxially overgrowing koksharovite, and as aggregates (up to 0.15 mm) associated with bannermanite in cavities in volcanic scoria. The mineral is translucent, yellowish-brown with an adamantine luster. The calculated density is 3.45 g cm
− 3
. In reflected light, ziminaite is light grey. Bireflectance is weak, internal reflections are deep yellow. The reflectance values [
R
max
–R
min
, % (λ, nm)] are: 17.7–16.3 (470), 15.7–14.1 (546), 15.1–13.8 (589), 14.7–13.6 (650). Chemical composition (wt%) is: MgO 2.20, CaO 0.01, Al
2
O
3
7.81, Fe
2
O
3
27.18, TiO
2
4.50, SiO
2
0.26, P
2
O
5
0.09, V
2
O
5
57.01, total 99.06. The empirical formula, based on 24 O atoms, is: (Fe
3 +
3.29
Al
1.48
Ti
0.54
Mg
0.53
)
Σ5.84
(V
6.05
Si
0.04
P
0.01
)
Σ6.10
O
24
(Z = 1). Ziminaite is triclinic,
P
1
¯
,
a
8.012(4),
b
9.345(5),
c
6.678(3) Å, α 106.992(10), β 101.547(8), γ 96.594(11)º,
V
460.4(4) Å
3
, Z = 6. The strongest reflections of the powder X-ray diffraction pattern [
d
,Å(
I
)(
hkl
)] are: 3.751(17)(1–21, 12 − 1), 3.539(86)(120), 3.270(67)(01–2), 3.209(100)(2–20), 3.090(20)(2–11, 002), 3.041(18)(03 − 1, 02–2), 2.934(14)(12 − 2, 030) and 1.665(24)(023, 12 − 4). The crystal structure, solved from single-crystal data (
R
1
= 0.085), is based upon heteropolyhedral framework built by VO
4
tetrahedra and Fe
3+
-centred octahedra and five-fold polyhedra. Ziminaite belongs to the howardevansite group being its first member without species-defining uni- or divalent cations and with all large cation sites vacant. The mineral is named after the Zimina volcano situated near the discovery locality.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00710-017-0550-y</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0930-0708 |
| ispartof | Mineralogy and petrology, 2018-06, Vol.112 (3), p.371-379 |
| issn | 0930-0708 1438-1168 |
| language | eng |
| recordid | cdi_proquest_journals_1972122373 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Aluminum oxide Cations Composition Crystal structure Crystals Diffraction Diffraction patterns Divalent cations Earth and Environmental Science Earth Sciences Frameworks Geochemistry Inorganic Chemistry Iron Luster Mineralogy Original Paper Polyhedra Reflectance Silicon dioxide Single crystals Titanium dioxide Vanadium pentoxide Volcanic activity Volcanoes X ray powder diffraction X-ray diffraction X-rays |
| title | Ziminaite, Fe3+VO4, a new howardevansite-group mineral from the Bezymyannyi volcano, Kamchatka, Russia |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-16T22%3A04%3A09IST&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=Ziminaite,%20Fe3+VO4,%20a%20new%20howardevansite-group%20mineral%20from%20the%20Bezymyannyi%20volcano,%20Kamchatka,%20Russia&rft.jtitle=Mineralogy%20and%20petrology&rft.au=Pekov,%20Igor%20V.&rft.date=2018-06-01&rft.volume=112&rft.issue=3&rft.spage=371&rft.epage=379&rft.pages=371-379&rft.issn=0930-0708&rft.eissn=1438-1168&rft_id=info:doi/10.1007/s00710-017-0550-y&rft_dat=%3Cproquest_cross%3E1972122373%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1972122373&rft_id=info:pmid/&rfr_iscdi=true |