A new mineral borisenkoite, Cu3[(V,As)O4]2, and the isomorphous series borisenkoite–lammerite-β in fumarolic exhalations of the Tolbachik volcano, Kamchatka, Russia
The new mineral borisenkoite Cu 3 [(V,As)O 4 ] 2 was found in sublimates of the Yadovitaya fumarole at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Associated minerals are sanidine, hematite, lammerite, lammerite-β...
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| creator | Pekov, Igor V. Zubkova, Natalia V. Yapaskurt, Vasiliy O. Polekhovsky, Yury S. Vigasina, Marina F. Britvin, Sergey N. Turchkova, Anna G. Sidorov, Evgeny G. Pushcharovsky, Dmitry Yu |
| description | The new mineral borisenkoite Cu
3
[(V,As)O
4
]
2
was found in sublimates of the Yadovitaya fumarole at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Associated minerals are sanidine, hematite, lammerite, lammerite-β, bradaczekite, zincobradaczekite, mcbirneyite, pseudolyonsite, lyonsite, starovaite, tenorite, rutile, tripuhyite, pseudobrookite, piypite, langbeinite, calciolangbeinite, aphthitalite, alumoklyuchevskite, palmierite, cupromolybdite, and corundum. Borisenkoite forms (1) prismatic crystals (up to 0.04 × 0.04 × 0.10 mm
3
) usually combined in clusters up to 0.4 mm and (2) rims up to 0.05 mm in width around lammerite. Borisenkoite is red-brown, golden-brown or brown, with strong greasy to adamantine lustre.
D
calc
is 4.69 g·cm
−3
. Chemical composition (wt.%, electron-microprobe) is: CuO 53.25, ZnO 1.13, Fe
2
O
3
0.16, P
2
O
5
0.05, V
2
O
5
25.06, As
2
O
5
20.44, total 100.07. The empirical formula, based on 8 O
apfu
, is: (Cu
2.94
Zn
0.06
Fe
0.01
)
Σ3.01
(V
1.21
As
0.78
)
Σ1.99
O
8
. Borisenkoite is monoclinic,
P
2
1
/
c
,
a
6.3779(7),
b
8.6021(9),
c
11.3597(11) Å, β 92.013(8)º,
V
622.84(11) Å
3
and
Z
= 4. The strongest reflections in the powder XRD pattern [
d
,Å(
I
)(
hkl
)] are: 4.309(48)(− 102, 020), 3.424(40)(022, − 121), 2.994(48)(113, 210), 2.917(50)(− 211), 2.830(100)(004), 2.782(92)(031) and 2.568(38)(123). The crystal structure was solved from single-crystal XRD data and refined to
R
= 0.0654. Borisenkoite is isotypic with lammerite-β. They form a limited solid-solution series extended from Cu
3
(AsO
4
)
2
to Cu
3
(V
1.5
As
0.5
)O
8
, with gap between Cu
3
(As
1.75
V
0.25
)O
8
and Cu
3
(As
1.25
V
0.75
)O
8
. The assumption that As
5+
can stabilize borisenkoite structure is the reason to propose the simplified formula Cu
3
[(V,As)O
4
]
2
avoiding the formal end-member formula Cu
3
(VO
4
)
2
. Borisenkoite is named in honour of the Russian geochemist, mineralogist, and geologist Leonid Fedorovich Borisenko (1922–2000). |
| doi_str_mv | 10.1007/s00269-020-01081-y |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2359482946</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2359482946</sourcerecordid><originalsourceid>FETCH-LOGICAL-c234y-cfdb5d038a54f99872ce8cff62910d4fb7f8f1875ad9c922434d06b288882bac3</originalsourceid><addsrcrecordid>eNp9kc-KFDEQxoMoOK6-gKeAF4WOVv70dOc4DKsrLizI6kUkpNOJnZ3uZEy6defmO_gQ3n0QH8InMe4I4sW61KG-76sqfgg9pPCUAjTPMgBbSwIMCFBoKTncQisqOCMMGL2NVsAFI7SR9C66l_MVQBk29Qp92-BgP-PJB5v0iLuYfLZhF_1sK7xd-LvHb6tNfnIh3rMK69DjebDY5zjFtB_iknG2ydv8j_Hnl6-jnqYymC358R37gN0y6RRHb7C9HvSoZx9DxtHdxF3GsdNm8Dv8KY5Gh1jhV3oyg553usKvl5y9vo_uOD1m--BPP0Fvnp9ebs_I-cWLl9vNOTGMiwMxru_qHnira-GkbBtmbGucWzNJoReua1zraNvUupdGMia46GHdsbYUK0fwE_TomLtP8eNi86yu4pJCWakYr6VomRTromJHlUkx52Sd2idfPjwoCuo3EHUEogoQdQNEHYqJH025iMMHm_5G_8f1Cz8kko4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2359482946</pqid></control><display><type>article</type><title>A new mineral borisenkoite, Cu3[(V,As)O4]2, and the isomorphous series borisenkoite–lammerite-β in fumarolic exhalations of the Tolbachik volcano, Kamchatka, Russia</title><source>SpringerLink Journals - AutoHoldings</source><creator>Pekov, Igor V. ; Zubkova, Natalia V. ; Yapaskurt, Vasiliy O. ; Polekhovsky, Yury S. ; Vigasina, Marina F. ; Britvin, Sergey N. ; Turchkova, Anna G. ; Sidorov, Evgeny G. ; Pushcharovsky, Dmitry Yu</creator><creatorcontrib>Pekov, Igor V. ; Zubkova, Natalia V. ; Yapaskurt, Vasiliy O. ; Polekhovsky, Yury S. ; Vigasina, Marina F. ; Britvin, Sergey N. ; Turchkova, Anna G. ; Sidorov, Evgeny G. ; Pushcharovsky, Dmitry Yu</creatorcontrib><description>The new mineral borisenkoite Cu
3
[(V,As)O
4
]
2
was found in sublimates of the Yadovitaya fumarole at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Associated minerals are sanidine, hematite, lammerite, lammerite-β, bradaczekite, zincobradaczekite, mcbirneyite, pseudolyonsite, lyonsite, starovaite, tenorite, rutile, tripuhyite, pseudobrookite, piypite, langbeinite, calciolangbeinite, aphthitalite, alumoklyuchevskite, palmierite, cupromolybdite, and corundum. Borisenkoite forms (1) prismatic crystals (up to 0.04 × 0.04 × 0.10 mm
3
) usually combined in clusters up to 0.4 mm and (2) rims up to 0.05 mm in width around lammerite. Borisenkoite is red-brown, golden-brown or brown, with strong greasy to adamantine lustre.
D
calc
is 4.69 g·cm
−3
. Chemical composition (wt.%, electron-microprobe) is: CuO 53.25, ZnO 1.13, Fe
2
O
3
0.16, P
2
O
5
0.05, V
2
O
5
25.06, As
2
O
5
20.44, total 100.07. The empirical formula, based on 8 O
apfu
, is: (Cu
2.94
Zn
0.06
Fe
0.01
)
Σ3.01
(V
1.21
As
0.78
)
Σ1.99
O
8
. Borisenkoite is monoclinic,
P
2
1
/
c
,
a
6.3779(7),
b
8.6021(9),
c
11.3597(11) Å, β 92.013(8)º,
V
622.84(11) Å
3
and
Z
= 4. The strongest reflections in the powder XRD pattern [
d
,Å(
I
)(
hkl
)] are: 4.309(48)(− 102, 020), 3.424(40)(022, − 121), 2.994(48)(113, 210), 2.917(50)(− 211), 2.830(100)(004), 2.782(92)(031) and 2.568(38)(123). The crystal structure was solved from single-crystal XRD data and refined to
R
= 0.0654. Borisenkoite is isotypic with lammerite-β. They form a limited solid-solution series extended from Cu
3
(AsO
4
)
2
to Cu
3
(V
1.5
As
0.5
)O
8
, with gap between Cu
3
(As
1.75
V
0.25
)O
8
and Cu
3
(As
1.25
V
0.75
)O
8
. The assumption that As
5+
can stabilize borisenkoite structure is the reason to propose the simplified formula Cu
3
[(V,As)O
4
]
2
avoiding the formal end-member formula Cu
3
(VO
4
)
2
. Borisenkoite is named in honour of the Russian geochemist, mineralogist, and geologist Leonid Fedorovich Borisenko (1922–2000).</description><identifier>ISSN: 0342-1791</identifier><identifier>EISSN: 1432-2021</identifier><identifier>DOI: 10.1007/s00269-020-01081-y</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Arsenic ions ; Chemical composition ; Cinder cones ; Corundum ; Crystal structure ; Crystallography and Scattering Methods ; Crystals ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Hematite ; Mineral Resources ; Mineralogy ; Organic chemistry ; Original Paper ; Phosphorus pentoxide ; Single crystals ; Solid solutions ; Volcanoes ; Zinc oxide</subject><ispartof>Physics and chemistry of minerals, 2020-03, Vol.47 (3), Article 17</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>2020© Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c234y-cfdb5d038a54f99872ce8cff62910d4fb7f8f1875ad9c922434d06b288882bac3</citedby><cites>FETCH-LOGICAL-c234y-cfdb5d038a54f99872ce8cff62910d4fb7f8f1875ad9c922434d06b288882bac3</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/s00269-020-01081-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00269-020-01081-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Pekov, Igor V.</creatorcontrib><creatorcontrib>Zubkova, Natalia V.</creatorcontrib><creatorcontrib>Yapaskurt, Vasiliy O.</creatorcontrib><creatorcontrib>Polekhovsky, Yury S.</creatorcontrib><creatorcontrib>Vigasina, Marina F.</creatorcontrib><creatorcontrib>Britvin, Sergey N.</creatorcontrib><creatorcontrib>Turchkova, Anna G.</creatorcontrib><creatorcontrib>Sidorov, Evgeny G.</creatorcontrib><creatorcontrib>Pushcharovsky, Dmitry Yu</creatorcontrib><title>A new mineral borisenkoite, Cu3[(V,As)O4]2, and the isomorphous series borisenkoite–lammerite-β in fumarolic exhalations of the Tolbachik volcano, Kamchatka, Russia</title><title>Physics and chemistry of minerals</title><addtitle>Phys Chem Minerals</addtitle><description>The new mineral borisenkoite Cu
3
[(V,As)O
4
]
2
was found in sublimates of the Yadovitaya fumarole at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Associated minerals are sanidine, hematite, lammerite, lammerite-β, bradaczekite, zincobradaczekite, mcbirneyite, pseudolyonsite, lyonsite, starovaite, tenorite, rutile, tripuhyite, pseudobrookite, piypite, langbeinite, calciolangbeinite, aphthitalite, alumoklyuchevskite, palmierite, cupromolybdite, and corundum. Borisenkoite forms (1) prismatic crystals (up to 0.04 × 0.04 × 0.10 mm
3
) usually combined in clusters up to 0.4 mm and (2) rims up to 0.05 mm in width around lammerite. Borisenkoite is red-brown, golden-brown or brown, with strong greasy to adamantine lustre.
D
calc
is 4.69 g·cm
−3
. Chemical composition (wt.%, electron-microprobe) is: CuO 53.25, ZnO 1.13, Fe
2
O
3
0.16, P
2
O
5
0.05, V
2
O
5
25.06, As
2
O
5
20.44, total 100.07. The empirical formula, based on 8 O
apfu
, is: (Cu
2.94
Zn
0.06
Fe
0.01
)
Σ3.01
(V
1.21
As
0.78
)
Σ1.99
O
8
. Borisenkoite is monoclinic,
P
2
1
/
c
,
a
6.3779(7),
b
8.6021(9),
c
11.3597(11) Å, β 92.013(8)º,
V
622.84(11) Å
3
and
Z
= 4. The strongest reflections in the powder XRD pattern [
d
,Å(
I
)(
hkl
)] are: 4.309(48)(− 102, 020), 3.424(40)(022, − 121), 2.994(48)(113, 210), 2.917(50)(− 211), 2.830(100)(004), 2.782(92)(031) and 2.568(38)(123). The crystal structure was solved from single-crystal XRD data and refined to
R
= 0.0654. Borisenkoite is isotypic with lammerite-β. They form a limited solid-solution series extended from Cu
3
(AsO
4
)
2
to Cu
3
(V
1.5
As
0.5
)O
8
, with gap between Cu
3
(As
1.75
V
0.25
)O
8
and Cu
3
(As
1.25
V
0.75
)O
8
. The assumption that As
5+
can stabilize borisenkoite structure is the reason to propose the simplified formula Cu
3
[(V,As)O
4
]
2
avoiding the formal end-member formula Cu
3
(VO
4
)
2
. Borisenkoite is named in honour of the Russian geochemist, mineralogist, and geologist Leonid Fedorovich Borisenko (1922–2000).</description><subject>Arsenic ions</subject><subject>Chemical composition</subject><subject>Cinder cones</subject><subject>Corundum</subject><subject>Crystal structure</subject><subject>Crystallography and Scattering Methods</subject><subject>Crystals</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Hematite</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Organic chemistry</subject><subject>Original Paper</subject><subject>Phosphorus pentoxide</subject><subject>Single crystals</subject><subject>Solid solutions</subject><subject>Volcanoes</subject><subject>Zinc oxide</subject><issn>0342-1791</issn><issn>1432-2021</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kc-KFDEQxoMoOK6-gKeAF4WOVv70dOc4DKsrLizI6kUkpNOJnZ3uZEy6defmO_gQ3n0QH8InMe4I4sW61KG-76sqfgg9pPCUAjTPMgBbSwIMCFBoKTncQisqOCMMGL2NVsAFI7SR9C66l_MVQBk29Qp92-BgP-PJB5v0iLuYfLZhF_1sK7xd-LvHb6tNfnIh3rMK69DjebDY5zjFtB_iknG2ydv8j_Hnl6-jnqYymC358R37gN0y6RRHb7C9HvSoZx9DxtHdxF3GsdNm8Dv8KY5Gh1jhV3oyg553usKvl5y9vo_uOD1m--BPP0Fvnp9ebs_I-cWLl9vNOTGMiwMxru_qHnira-GkbBtmbGucWzNJoReua1zraNvUupdGMia46GHdsbYUK0fwE_TomLtP8eNi86yu4pJCWakYr6VomRTromJHlUkx52Sd2idfPjwoCuo3EHUEogoQdQNEHYqJH025iMMHm_5G_8f1Cz8kko4</recordid><startdate>20200301</startdate><enddate>20200301</enddate><creator>Pekov, Igor V.</creator><creator>Zubkova, Natalia V.</creator><creator>Yapaskurt, Vasiliy O.</creator><creator>Polekhovsky, Yury S.</creator><creator>Vigasina, Marina F.</creator><creator>Britvin, Sergey N.</creator><creator>Turchkova, Anna G.</creator><creator>Sidorov, Evgeny G.</creator><creator>Pushcharovsky, Dmitry Yu</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20200301</creationdate><title>A new mineral borisenkoite, Cu3[(V,As)O4]2, and the isomorphous series borisenkoite–lammerite-β in fumarolic exhalations of the Tolbachik volcano, Kamchatka, Russia</title><author>Pekov, Igor V. ; Zubkova, Natalia V. ; Yapaskurt, Vasiliy O. ; Polekhovsky, Yury S. ; Vigasina, Marina F. ; Britvin, Sergey N. ; Turchkova, Anna G. ; Sidorov, Evgeny G. ; Pushcharovsky, Dmitry Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c234y-cfdb5d038a54f99872ce8cff62910d4fb7f8f1875ad9c922434d06b288882bac3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Arsenic ions</topic><topic>Chemical composition</topic><topic>Cinder cones</topic><topic>Corundum</topic><topic>Crystal structure</topic><topic>Crystallography and Scattering Methods</topic><topic>Crystals</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Hematite</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Organic chemistry</topic><topic>Original Paper</topic><topic>Phosphorus pentoxide</topic><topic>Single crystals</topic><topic>Solid solutions</topic><topic>Volcanoes</topic><topic>Zinc oxide</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pekov, Igor V.</creatorcontrib><creatorcontrib>Zubkova, Natalia V.</creatorcontrib><creatorcontrib>Yapaskurt, Vasiliy O.</creatorcontrib><creatorcontrib>Polekhovsky, Yury S.</creatorcontrib><creatorcontrib>Vigasina, Marina F.</creatorcontrib><creatorcontrib>Britvin, Sergey N.</creatorcontrib><creatorcontrib>Turchkova, Anna G.</creatorcontrib><creatorcontrib>Sidorov, Evgeny G.</creatorcontrib><creatorcontrib>Pushcharovsky, Dmitry Yu</creatorcontrib><collection>CrossRef</collection><jtitle>Physics and chemistry of minerals</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pekov, Igor V.</au><au>Zubkova, Natalia V.</au><au>Yapaskurt, Vasiliy O.</au><au>Polekhovsky, Yury S.</au><au>Vigasina, Marina F.</au><au>Britvin, Sergey N.</au><au>Turchkova, Anna G.</au><au>Sidorov, Evgeny G.</au><au>Pushcharovsky, Dmitry Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A new mineral borisenkoite, Cu3[(V,As)O4]2, and the isomorphous series borisenkoite–lammerite-β in fumarolic exhalations of the Tolbachik volcano, Kamchatka, Russia</atitle><jtitle>Physics and chemistry of minerals</jtitle><stitle>Phys Chem Minerals</stitle><date>2020-03-01</date><risdate>2020</risdate><volume>47</volume><issue>3</issue><artnum>17</artnum><issn>0342-1791</issn><eissn>1432-2021</eissn><abstract>The new mineral borisenkoite Cu
3
[(V,As)O
4
]
2
was found in sublimates of the Yadovitaya fumarole at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Associated minerals are sanidine, hematite, lammerite, lammerite-β, bradaczekite, zincobradaczekite, mcbirneyite, pseudolyonsite, lyonsite, starovaite, tenorite, rutile, tripuhyite, pseudobrookite, piypite, langbeinite, calciolangbeinite, aphthitalite, alumoklyuchevskite, palmierite, cupromolybdite, and corundum. Borisenkoite forms (1) prismatic crystals (up to 0.04 × 0.04 × 0.10 mm
3
) usually combined in clusters up to 0.4 mm and (2) rims up to 0.05 mm in width around lammerite. Borisenkoite is red-brown, golden-brown or brown, with strong greasy to adamantine lustre.
D
calc
is 4.69 g·cm
−3
. Chemical composition (wt.%, electron-microprobe) is: CuO 53.25, ZnO 1.13, Fe
2
O
3
0.16, P
2
O
5
0.05, V
2
O
5
25.06, As
2
O
5
20.44, total 100.07. The empirical formula, based on 8 O
apfu
, is: (Cu
2.94
Zn
0.06
Fe
0.01
)
Σ3.01
(V
1.21
As
0.78
)
Σ1.99
O
8
. Borisenkoite is monoclinic,
P
2
1
/
c
,
a
6.3779(7),
b
8.6021(9),
c
11.3597(11) Å, β 92.013(8)º,
V
622.84(11) Å
3
and
Z
= 4. The strongest reflections in the powder XRD pattern [
d
,Å(
I
)(
hkl
)] are: 4.309(48)(− 102, 020), 3.424(40)(022, − 121), 2.994(48)(113, 210), 2.917(50)(− 211), 2.830(100)(004), 2.782(92)(031) and 2.568(38)(123). The crystal structure was solved from single-crystal XRD data and refined to
R
= 0.0654. Borisenkoite is isotypic with lammerite-β. They form a limited solid-solution series extended from Cu
3
(AsO
4
)
2
to Cu
3
(V
1.5
As
0.5
)O
8
, with gap between Cu
3
(As
1.75
V
0.25
)O
8
and Cu
3
(As
1.25
V
0.75
)O
8
. The assumption that As
5+
can stabilize borisenkoite structure is the reason to propose the simplified formula Cu
3
[(V,As)O
4
]
2
avoiding the formal end-member formula Cu
3
(VO
4
)
2
. Borisenkoite is named in honour of the Russian geochemist, mineralogist, and geologist Leonid Fedorovich Borisenko (1922–2000).</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00269-020-01081-y</doi></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0342-1791 |
| ispartof | Physics and chemistry of minerals, 2020-03, Vol.47 (3), Article 17 |
| issn | 0342-1791 1432-2021 |
| language | eng |
| recordid | cdi_proquest_journals_2359482946 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Arsenic ions Chemical composition Cinder cones Corundum Crystal structure Crystallography and Scattering Methods Crystals Earth and Environmental Science Earth Sciences Geochemistry Hematite Mineral Resources Mineralogy Organic chemistry Original Paper Phosphorus pentoxide Single crystals Solid solutions Volcanoes Zinc oxide |
| title | A new mineral borisenkoite, Cu3[(V,As)O4]2, and the isomorphous series borisenkoite–lammerite-β in fumarolic exhalations of the Tolbachik 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=2024-12-30T23%3A12%3A13IST&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=A%20new%20mineral%20borisenkoite,%20Cu3%5B(V,As)O4%5D2,%20and%20the%20isomorphous%20series%20borisenkoite%E2%80%93lammerite-%CE%B2%20in%20fumarolic%20exhalations%20of%20the%20Tolbachik%20volcano,%20Kamchatka,%20Russia&rft.jtitle=Physics%20and%20chemistry%20of%20minerals&rft.au=Pekov,%20Igor%20V.&rft.date=2020-03-01&rft.volume=47&rft.issue=3&rft.artnum=17&rft.issn=0342-1791&rft.eissn=1432-2021&rft_id=info:doi/10.1007/s00269-020-01081-y&rft_dat=%3Cproquest_cross%3E2359482946%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=2359482946&rft_id=info:pmid/&rfr_iscdi=true |