Rare earth element content in the Szentbékkála series of peridotite inclusions
The genetic relations of four nonfrequent xenolith inclusion groups (dunite, layered lherzolite, websteriteandspinel-pyroxenite) to the hypothetical mantle sourcespinel-lherzolite(themostfrequent inclusion) and to the host alkali basalts have been investigated. The concentrations of rare-earth eleme...
Elmentve itt :
| Szerzők: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1986
|
| Sorozat: | Acta mineralogica-petrographica
28 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24749 |
| LEADER | 02207nab a2200229 i 4500 | ||
|---|---|---|---|
| 001 | acta24749 | ||
| 005 | 20220726130925.0 | ||
| 008 | 161017s1986 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Bérczi Szaniszló | |
| 245 | 1 | 0 | |a Rare earth element content in the Szentbékkála series of peridotite inclusions |h [elektronikus dokumentum] / |c Bérczi Szaniszló |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1986 | ||
| 300 | |a 61-74 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 28 | |
| 520 | 3 | |a The genetic relations of four nonfrequent xenolith inclusion groups (dunite, layered lherzolite, websteriteandspinel-pyroxenite) to the hypothetical mantle sourcespinel-lherzolite(themostfrequent inclusion) and to the host alkali basalts have been investigated. The concentrations of rare-earth elements (REE) in the basalts, in the peridotite inclusions and in the mineral separates of spinellherzolites and spinel-pyroxenites were determined by instrumental neutron activation analysis. The REE abundance patterns of peridotite inclusions show increasing REE concentrations in the order: dunite, spinel-lherzolite, layered lherzolite, websterite and spinel-pyroxenite. Except spinelpyroxenite this series of inclusions represents a gradation from depleted (the former two groups) to enriched (the later two groups) remnants of source mantle material. The enrichment of REE in spinel-pyroxenites and alkali basalts are in accord with their 17 percent and 3 percent partial melting from a chondritic mantle source. On the basis of our REE concentration measurements on alkali basalts containing peridotite inclusions (Szigliget, Szentbékkálla, Kapolcs) we suggest the introduction of a new group, the peridotite inclusion containing basalt group into GY . PANTÓ'S classification of Hungarian basalts. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 700 | 0 | 1 | |a Bérczi János |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24749/1/mineralogica_028_061-074.pdf |z Dokumentum-elérés |