Hydrothermal-to-metasomatic overprint of the neovolcanic rocks
evidenced by composite apatite crystals: A case study from the
Maglovec Hill, Slanské vrchy Mountains, Slovakia

J 2018

Hydrothermal-to-metasomatic overprint of the neovolcanic rocks evidenced by composite apatite crystals: A case study from the Maglovec Hill, Slanské vrchy Mountains, Slovakia

NOEMI, Mészárosová; Skála ROMAN; Matoušková ŠÁRKA; Petr MIKYSEK; Plášil JAKUB et al.

Základní údaje

Originální název

Hydrothermal-to-metasomatic overprint of the neovolcanic rocks evidenced by composite apatite crystals: A case study from the Maglovec Hill, Slanské vrchy Mountains, Slovakia

Autoři

NOEMI, Mészárosová; Skála ROMAN; Matoušková ŠÁRKA; Petr MIKYSEK; Plášil JAKUB a Císařová IVANA

Vydání

Geologica Carpathica, 2018, 1335-0552

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Slovensko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.699

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/18:00105914

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

hydrothermal alteration; crystal chemistry; apatite; REE; SCXRD; PXRD; EPMA; SEM; LA–ICP–MS; Raman spectroscopy

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 30. 4. 2020 10:07, Mgr. Petr Mikysek, Ph.D.

Anotace

V originále

The apatite assemblage from Maglovec hill (Slanské vrchy Mountains near the city of Prešov) from fissures of hydrothermally altered neovolcanic rocks (andesites and related lithologies) was studied. The assemblage consists of two different morphological apatite types (apatite in cores of prismatic crystals and fibrous apatite mantling these cores). The assemblage was investigated by a multi analytical approach to reveal its unique chemical composition and structure. The acquired data suggest a hydrothermal origin of this assemblage and indicate a formation sequence of distinct apatite types. Moreover, minerals from the epidote group were identified, which have not been described from this locality before as well as vanadium-rich magnetites that form exsolution lamellae in ilmenite grains.

Citovat

NOEMI, Mészárosová; Skála ROMAN; Matoušková ŠÁRKA; Petr MIKYSEK; Plášil JAKUB a Císařová IVANA. Hydrothermal-to-metasomatic overprint of the neovolcanic rocks evidenced by composite apatite crystals: A case study from the Maglovec Hill, Slanské vrchy Mountains, Slovakia. Geologica Carpathica. 2018, roč. 69, č. 5, s. 439-452. ISSN 1335-0552. Dostupné z: https://doi.org/10.1515/geoca-2018-0025.

@article{1490873,
   author = {Noemi, Mészárosová and Roman, Skála and Šárka, Matoušková and Mikysek, Petr and Jakub, Plášil and Ivana, Císařová},
   article_number = {5},
   doi = {https://doi.org/10.1515/geoca-2018-0025},
   keywords = {hydrothermal alteration; crystal chemistry; apatite; REE; SCXRD; PXRD; EPMA; SEM; LA–ICP–MS; Raman spectroscopy},
   language = {eng},
   issn = {1335-0552},
   journal = {Geologica Carpathica},
   title = {Hydrothermal-to-metasomatic overprint of the neovolcanic rocks evidenced by composite apatite crystals: A case study from the Maglovec Hill, Slanské vrchy Mountains, Slovakia},
   url = {https://content.sciendo.com/view/journals/geoca/69/5/article-p439.xml},
   volume = {69},
   year = {2018}
}

TY  - JOUR
ID  - 1490873
AU  - Noemi, Mészárosová - Roman, Skála - Šárka, Matoušková - Mikysek, Petr - Jakub, Plášil - Ivana, Císařová
PY  - 2018
TI  - Hydrothermal-to-metasomatic overprint of the neovolcanic rocks evidenced by composite apatite crystals: A case study from the Maglovec Hill, Slanské vrchy Mountains, Slovakia
JF  - Geologica Carpathica
VL  - 69
IS  - 5
SP  - 439-452
EP  - 439-452
SN  - 13350552
KW  - hydrothermal alteration
KW  - crystal chemistry
KW  - apatite
KW  - REE
KW  - SCXRD
KW  - PXRD
KW  - EPMA
KW  - SEM
KW  - LA–ICP–MS
KW  - Raman spectroscopy
UR  - https://content.sciendo.com/view/journals/geoca/69/5/article-p439.xml
L2  - https://content.sciendo.com/view/journals/geoca/69/5/article-p439.xml
N2  - The apatite assemblage from Maglovec hill (Slanské vrchy Mountains near the city of Prešov) from fissures of hydrothermally altered neovolcanic rocks (andesites and related lithologies) was studied. The assemblage consists of two different morphological apatite types (apatite in cores of prismatic crystals and fibrous apatite mantling these cores). The assemblage was investigated by a multi analytical approach to reveal its unique chemical composition and structure. The acquired data suggest a hydrothermal origin of this assemblage and indicate a formation sequence of distinct apatite types. Moreover, minerals from the epidote group were identified, which have not been described from this locality before as well as vanadium-rich magnetites that form exsolution lamellae in ilmenite grains.
ER  -

NOEMI, Mészárosová; Skála ROMAN; Matoušková ŠÁRKA; Petr MIKYSEK; Plášil JAKUB a Císařová IVANA. Hydrothermal-to-metasomatic overprint of the neovolcanic rocks evidenced by composite apatite crystals: A case study from the Maglovec Hill, Slanské vrchy Mountains, Slovakia. \textit{Geologica Carpathica}. 2018, roč.~69, č.~5, s.~439-452. ISSN~1335-0552. Dostupné z: https://doi.org/10.1515/geoca-2018-0025.

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