2012
Sapphires related to alkali basalts from the Cerová Highlands, Western Carpathians (southern Slovakia): composition and origin
UHER, Pavel; Gaston GIULIANI; Sandor SZÁKALL; Anthony FALLICK; Vladimír STRUNGA et al.Základní údaje
Originální název
Sapphires related to alkali basalts from the Cerová Highlands, Western Carpathians (southern Slovakia): composition and origin
Autoři
UHER, Pavel; Gaston GIULIANI; Sandor SZÁKALL; Anthony FALLICK; Vladimír STRUNGA; Tomáš VACULOVIČ; Daniel OZDÍN a Markéta GREGÁŇOVÁ
Vydání
Geologica Carpathica, Bratislava, Slovak Akademy Press, 2012, 1335-0552
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10406 Analytical chemistry
Stát vydavatele
Slovensko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 1.143
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14740/12:00060079
Organizační jednotka
Středoevropský technologický institut
UT WoS
Klíčová slova anglicky
Western Carpathians; Slovakia; Hajnáčka; Gortva; CL; LA-ICP-MS; EMPA; oxygen isotopes; placer; alkali basalts; anorthoclasite xenolith; corundum; sapphire
Změněno: 11. 4. 2013 10:36, Olga Křížová
Anotace
V originále
Blue, grey-pink and pink sapphires from the Cerová Highlands, Western Carpathians (southern Slovakia) have been studied using CL, LA-ICP-MS, EMPA, and oxygen isotope methods. The sapphire occurs as (1) clastic heavy mineral in the secondary sandy filling of a Pliocene alkali basaltic maar at Hajnáčka, and (2) crystals in a pyroxenebearing syenite/anorthoclasite xenolith of Pleistocene alkali basalt near Gortva. Critical evaluation of compositional diagrams (Fe, Ti, Cr, Ga, Mg contents, Fe/Ti, Cr/Ga, Ga/Mg ratios) suggests a magmatic origin for clastic blue sapphires with lower Cr and Mg, but higher Fe and Ti concentrations in comparison to the grey-pink and pink varietes, as well as similar compositional trends with blue sapphire from the Gortva magmatic xenolith. Moreover, blue sapphires show similar 18O values: 5.1 in the Gortva xenolith, 3.8 and 5.85 in the Hajnáčka placer, closely comparable to mantle to lower crustal magmatic rocks. On the contrary, pink and grey-pink sapphires show higher Cr and Mg, but lower Fe and Ti contents and their composition points to a metamorphic (metasomatic) origin.
Návaznosti
| MSM0021622411, záměr |
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| MUNI/G/0124/2009, interní kód MU |
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