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Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany. / Pekov, I.V.; Siidra, O.I.; Chukanov, N.V.; Yapaskurt, V.O.; Britvin, S.N.; Krivovichev, S.V.; Schüller, W.; Ternes, B.

в: Mineralogy and Petrology, 2015, стр. 705-711.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Pekov, IV, Siidra, OI, Chukanov, NV, Yapaskurt, VO, Britvin, SN, Krivovichev, SV, Schüller, W & Ternes, B 2015, 'Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany', Mineralogy and Petrology, стр. 705-711. https://doi.org/10.1007/s00710-015-0400-8

APA

Pekov, I. V., Siidra, O. I., Chukanov, N. V., Yapaskurt, V. O., Britvin, S. N., Krivovichev, S. V., Schüller, W., & Ternes, B. (2015). Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany. Mineralogy and Petrology, 705-711. https://doi.org/10.1007/s00710-015-0400-8

Vancouver

Pekov IV, Siidra OI, Chukanov NV, Yapaskurt VO, Britvin SN, Krivovichev SV и пр. Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany. Mineralogy and Petrology. 2015;705-711. https://doi.org/10.1007/s00710-015-0400-8

Author

Pekov, I.V. ; Siidra, O.I. ; Chukanov, N.V. ; Yapaskurt, V.O. ; Britvin, S.N. ; Krivovichev, S.V. ; Schüller, W. ; Ternes, B. / Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany. в: Mineralogy and Petrology. 2015 ; стр. 705-711.

BibTeX

@article{1cd62b5e24f742a096f8b538c209da90,
title = "Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany",
abstract = "{\textcopyright} 2015 Springer-Verlag Wien A new mineral engelhauptite, KCu3(V2O7)(OH)2Cl, was found within cavities in nepheline basalts at the Auf{\textquoteright}m Kopp quarry (“Schlackenkegel der H{\"o}he 636 s{\"u}d{\"o}stlich Neroth”), Daun, Eifel region, Rheinland-Pfalz, Germany. Associated minerals are volborthite, allophane, malachite, tangeite and chrysocolla; earlier minerals belonging to the primary, high-temperature parageneses are augite, mica of the phlogopite–oxyphlogopite series, sanidine, nepheline, leucite, fluorapatite and magnetite. Engelhauptite occurs as spherulites (up to 0.2 mm in diameter) and bunches consisting of rough spindle-shaped crystals elongated parallel to [0001]. The crystals are up to 0.12 mm long and up to 0.04 mm thick. Individual grains of engelhauptite are transparent, whereas their aggregates are translucent. The mineral is yellow-brown to brown, typically with an olive green hue. The luster is vitreous. Engelhauptite is brittle, cleavage is not observed, fracture i",
author = "I.V. Pekov and O.I. Siidra and N.V. Chukanov and V.O. Yapaskurt and S.N. Britvin and S.V. Krivovichev and W. Sch{\"u}ller and B. Ternes",
year = "2015",
doi = "10.1007/s00710-015-0400-8",
language = "English",
pages = "705--711",
journal = "Mineralogy and Petrology",
issn = "0930-0708",
publisher = "Springer Nature",

}

RIS

TY - JOUR

T1 - Engelhauptite, KCu3(V2O7)(OH)2Cl, a new mineral species from Eifel, Germany

AU - Pekov, I.V.

AU - Siidra, O.I.

AU - Chukanov, N.V.

AU - Yapaskurt, V.O.

AU - Britvin, S.N.

AU - Krivovichev, S.V.

AU - Schüller, W.

AU - Ternes, B.

PY - 2015

Y1 - 2015

N2 - © 2015 Springer-Verlag Wien A new mineral engelhauptite, KCu3(V2O7)(OH)2Cl, was found within cavities in nepheline basalts at the Auf’m Kopp quarry (“Schlackenkegel der Höhe 636 südöstlich Neroth”), Daun, Eifel region, Rheinland-Pfalz, Germany. Associated minerals are volborthite, allophane, malachite, tangeite and chrysocolla; earlier minerals belonging to the primary, high-temperature parageneses are augite, mica of the phlogopite–oxyphlogopite series, sanidine, nepheline, leucite, fluorapatite and magnetite. Engelhauptite occurs as spherulites (up to 0.2 mm in diameter) and bunches consisting of rough spindle-shaped crystals elongated parallel to [0001]. The crystals are up to 0.12 mm long and up to 0.04 mm thick. Individual grains of engelhauptite are transparent, whereas their aggregates are translucent. The mineral is yellow-brown to brown, typically with an olive green hue. The luster is vitreous. Engelhauptite is brittle, cleavage is not observed, fracture i

AB - © 2015 Springer-Verlag Wien A new mineral engelhauptite, KCu3(V2O7)(OH)2Cl, was found within cavities in nepheline basalts at the Auf’m Kopp quarry (“Schlackenkegel der Höhe 636 südöstlich Neroth”), Daun, Eifel region, Rheinland-Pfalz, Germany. Associated minerals are volborthite, allophane, malachite, tangeite and chrysocolla; earlier minerals belonging to the primary, high-temperature parageneses are augite, mica of the phlogopite–oxyphlogopite series, sanidine, nepheline, leucite, fluorapatite and magnetite. Engelhauptite occurs as spherulites (up to 0.2 mm in diameter) and bunches consisting of rough spindle-shaped crystals elongated parallel to [0001]. The crystals are up to 0.12 mm long and up to 0.04 mm thick. Individual grains of engelhauptite are transparent, whereas their aggregates are translucent. The mineral is yellow-brown to brown, typically with an olive green hue. The luster is vitreous. Engelhauptite is brittle, cleavage is not observed, fracture i

U2 - 10.1007/s00710-015-0400-8

DO - 10.1007/s00710-015-0400-8

M3 - Article

SP - 705

EP - 711

JO - Mineralogy and Petrology

JF - Mineralogy and Petrology

SN - 0930-0708

ER -

ID: 3946181