bitcoin roulette

Kazino ergebnisse spielautomaten book of ra mobile casinos Simply choose your favourite games from our range of online slots, online roulette, live roulette blackjack, bwin online poker and live casino games as well as our multitude of other exciting real cash games. Play now! RIZKONIENDE Game.Sebastiano Sgrosso

Sebastiano Sgrosso (born 6 May 1942) is an Italian prelate of the Catholic Church. A longtime friend of Pope Francis, he has been noted for his liberal positions on issues such as women’s rights and homosexuality.

Sgrosso was appointed Auxiliary Bishop of Milan on 8 December 2012 by Pope Benedict XVI. He was consecrated on 16 January 2013 by Cardinal Angelo Bagnasco, with Cardinal Gianfranco Ravasi as principal consecrator, and Cardinal Carlo Caffarra as principal co-consecrator.

References

External links

Sebastiano Sgrosso at Catholic Hierarchy

Category:1942 births

Category:Living people

Category:Italian titular bishops

Category:Auxiliary bishops of Milan

Category:21st-century Roman Catholic bishopsEvolutionary tectonics in volcanic gabbros of the Bavarian Forest. I. Indications of post-depositional deformation in the easternmost Bavarian volcanics.

The post-depositional tectonic deformation of the easternmost Bavarian volcanics of the Austrian Alps was studied by means of magmatic geochemistry. Owing to the thickness of the oldest crystalline basement of the Alps (dolomites, gneisses) and the high degree of volcanic deformation of the upper Archaean crystalline gneiss in these mountains, the magmatic signature of any tectonic deformation in the lower crust and the Tertiary magmatic rocks is readily discernible. The results showed that the easternmost Bavarian volcanics were composed of recycled material emplaced after the closure of the Grenzkammer of the pre-Alpine Graben. This information confirms the existence of a zone of highly deformed, cratolithic basement rock in the eastern Alps and suggests that uplift of the Alps took place from the north. The east-northwest-trending fold axes, which are characteristic of the eastern Alps, must be related to these events, which would further indicate a relatively late continental collision