Detailed Information on Publication Record
2014
Iron plus magnesium-bearing beryl from granitic pegmatites: an EMPA, LA-ICP-MS, Mossbauer spectroscopy, and powder XRD study
PŘIKRYL, Jan, Milan NOVÁK, Jan FILIP, Petr GADAS, Michaela VAŠINOVÁ GALIOVÁ et. al.Basic information
Original name
Iron plus magnesium-bearing beryl from granitic pegmatites: an EMPA, LA-ICP-MS, Mossbauer spectroscopy, and powder XRD study
Name in Czech
Železem a hořčíkem obohacený beryl z granitických pegmatitů: EMPA, LA-ICP-MS, Mossbauerova spektroskopie a prášková RTG difrakční studie
Authors
PŘIKRYL, Jan (203 Czech Republic, guarantor, belonging to the institution), Milan NOVÁK (203 Czech Republic, belonging to the institution), Jan FILIP (203 Czech Republic), Petr GADAS (203 Czech Republic, belonging to the institution) and Michaela VAŠINOVÁ GALIOVÁ (203 Czech Republic, belonging to the institution)
Edition
Canadian Mineralogist, QUEBEC, Mineralogical Association of Canada. 2014, 0008-4476
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Canada
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 1.181
RIV identification code
RIV/00216224:14310/14:00074475
Organization unit
Faculty of Science
UT WoS
000339701800009
Keywords (in Czech)
beryl; železo; hořčík; EMPA; LA-ICP-MS; Mossbauerova spektroskopie; granitické pegmatity
Keywords in English
beryl; iron; magnesium; EMPA; LA-ICP-MS; Mossbauer spectroscopy; granitic pegmatites
Tags
Tags
International impact, Reviewed
Změněno: 28/4/2015 09:55, Ing. Andrea Mikešková
Abstract
V originále
Five samples of blue, bluish green, and green Fe,Mg-enriched beryl from Li-poor granitic pegmatites [beryl-columbite (LCT) pegmatites at Kovarova and Bonenov in the Czech Republic and Val Sissone in Italy; a primitive pegmatite at Beryller, Untersulzbachtal, Austria; and a euxenite (NYF) pegmatite from the Beryl Pit, Quadeville, Ontario] were investigated using EMPA, Mossbauer spectroscopy, LA-ICP-MS, and powder XRD diffraction. The EMPA data show highly heterogeneous (Kovarova, Val Sissone) to rather homogeneous crystals (Bonenov, Beryller, Quadeville), with high variations in Al (1.51-1.91 apfu), Mg (0.01-0.31), Fe-tot (0.01-0.18), and Na (0.04-0.37). The substitution (CH)square + R-O(3+) <-> R-CH(+) + R-O(2+) is dominant and supported by the powder XRD data. LA-ICP-MS revealed notable concentrations of some trace elements: Cs <= 7568 ppm (Kovarova), Li <= 928 ppm (Quadeville), Sc <= 2823 ppm (Val Sissone). Beryl samples have mostly comparable contents of Fe3+, similar to 25% at the O-site, but differ in the presence of Fe2+ at the T(2)-site. Primitive characteristics of some examined beryl (Mg/(Mg+Fe-tot) = 0.37-0.68 reflect low degree of fractionation of the host pegmatite (Beryller), or high degree of Mg-contamination from host metabasites in the pegmatite dikes (Kovarova, Bonenov). The concentrations and ratios of selected elements, including Fe3+/Fe2+, in beryl from these Li-poor pegmatites are not feasible for any implications of pegmatite-family affinity or degree of its fractionation except for Li; however, no evident correlation between Li and Cs contents was found.
Links
| ED1.1.00/02.0068, research and development project |
| ||
| GAP210/10/0743, research and development project |
|