 |
| Titel |
A geochemical study of alkaline and tholeitic lavas from the Hyblean Plateau (Italy): inferences from noble gases, trace elements and Sr-Nd isotopes |
| VerfasserIn |
Alessandra Correale, Mauro Martelli, Antonio Paonita, Andrea Luca Rizzo, Vittorio Scribano, Ilenia Arienzo |
| Konferenz |
EGU General Assembly 2017
|
| Medientyp |
Artikel
|
| Sprache |
en
|
| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 19 (2017) |
| Datensatznummer |
250152766
|
| Publikation (Nr.) |
 EGU/EGU2017-17647.pdf |
|
|
|
|
|
| Zusammenfassung |
| Eight Plio-Pleistocenic lavas from the Hyblean volcanic province, south-eastern Sicily
(Italy), were investigated for the noble gas geochemistry, for the first time. Major
element composition classified these products as tholeiite basalts, basanites and
nephelinites. Noble gas content of fluid inclusions from their olivine and/or orthopyroxene
phenocrysts was analyzed for He, Ne and Ar and ranges between 45×10−15–3.78×10−11,
2.12×10−16–1.13×10−14 and 5.13×10−13–4.48×10−11 mol/g, respectively. Most samples
display 3He/4He ratios of about 7Ra (where Ra is the atmospheric 3He/4He ratio of
1.38×10−6) except for two lavas characterized by low He abundance and showing 3He/4He
= 3.53 and 8.35Ra, respectively. Such a wide deviation from the most recurrent value (7Ra) is
attributed to external inputs of 4He and 3He by secondary phenomena (i.e. magma aging,
crustal contamination and cosmogenic processes, respectively). The isotopic signature of He,
together with Sr and Nd isotope data (87Sr/86Sr=0.70274-0.70331; 143Nd/144Nd
=0,51293-0,513162) evidenced a strict relation with mantle harzburgite xenoliths
found in Miocenic diatremes from the same volcanic province, suggesting that a
depleted mantle source with an 3He/4He of about 7Ra fed the Plio-Pleistocenic
volcanism.
In this respect, the wide compositional spectrum of the samples, ranging from nephelinite
to tholeiite, could derive from the different P-T conditions during partial melting and/or
different partial melting degrees of this common mantle source. Contrarily, trace elements did
not highlight the close relation between the Plio-Pleistocenic lavas and mantle xenoliths
from diatremes, as cryptic metasomatism seems to modify the primordial trace
elements feature of xenoliths after their entrapment in the diatreme eruptive systems. |
|
|
|
|
|
|