1,354,502 research outputs found
Some constraints on geochemical features in the Triassic mantle of the easternmost austroalpine-southalpine domain: evidence from the Karawanken pluton (Carinthia, Austria)
No full textThe Karawanken pluton, near Eisenkappel
(Carinthia, Austria), is composed of closely alternating,
E/W-running, essentially granitic and dioritic
bands, with minor gabbro, monzonite, and hybrid
rocks, and is cut by diabase dykes. This pluton, of Triassic
age, is a shallow-emplaced intrusion, the rocks of
which belong to a series of alkaline affinity and,
despite local evidence of mixing and mingling of magmas,
the bulk of the pluton in the examined area
evolved mainly by fractional crystallization. The shift
in the initial Sr isotope ratio from gabbro (0.70313) to
monzonite (0.70525) and steady values from monzonite
to granite (0.70473) suggest a predominant assimilation
and fractional crystallization (AFC) process in
the mafic stage, followed by a dominant fractional
crystallization (FC) process when residual liquids
became felsic. The geochemical characteristics of the
Karawanken pluton point to a mantle source enriched
both in LILE and HFSE, whereas the coeval magmas
of the nearby Dolomites (NE Italy), emplaced in the
same extensional±transtensional geodynamic framework,
derive from a mantle modified by preceding
(Variscan) subductive processes. These geochemical
differences in the Triassic mantle of this part of the
Eastern Alps may involve the different Paleozoic geodynamic
evolution of these two sectors, e.g., the fact
that they belong to two different microplates linked in
the Middle Carboniferous. In any case, both the magmas
of the Karawanken pluton and of the Dolomites
clearly fit the mid-Triassic transtensional±extensional
tectonism which acted in the Southalpine±Austroalpine
and Dinaric domains during the initial stages of
Mesozoic rifting
“I will never again drink of the fruit of the vine until...”: Last Supper and eschatological meal in Mk 14,25
No full textThe logion on the "fruit of the vine" (Mk 14:25), wich contrasts with the context of the narratives of “institution of the Eucharist”, which in turn attest to a ritualization of the Eucharist as the memorial of the Lord's passion and meal for the intermediate time, "until he comes" (I Cor 11:26), is most likely an authentic saying of Jesus that preserves track of a fervent expectation of the imminent irruption of the kingdom of God, and perhaps refers to a conception of the Eucharist as an anticipation of the eschatological banquet in the kingdom.
Mk 14:25 remains extraneous to the Eucharistic anaphora and formulas of the ancient liturgies, while survives in millenarian contexts, such as expectation of an eschatological banquet with the risen Lord. This ‘materialistic’ perspective was neutralized by the spiritualistic interpretation of Origen and gradually absorbed by the prevailing ecclesiological conception that the feast of the kingdom, in which you drink the new wine, is precisely the Eucharistic celebration of the church: the eschatological horizon appears thus profoundly changed
The epiplutonic Hercynian Complex of Bressanone (Brixen, Eastern Alps, Italy). Petrologic and radiometric data
No full text
New geochemical and petrographic data on the Gabbro-Syenite Suite between Hargeisa and Berbera-Shiik (Northern Somalia).
No full textRecensione a: A. Rudolph, 'Denn wir sind jenes Volk...'. Die neue Gottesverehrung in Justins Dialog mit dem Juden Tryphon in historish-theologischer Sicht (Hereditas. Studien zur Alten Kirchengeschichte, 15)
No full textLo stock di granito a cordierite del M. Sella nel Massiccio di Bressanone (Alpi Orientali)
No full textRecensione a: An Diognet, übersetz und erklärt von Horacio E. Lona (Kommentar zu frühchristlichen Apologeten, 8), Freiburg 2001
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