Add to ORKGAn occurrence of the rare mineral tuhualite (NaFe3+Fe2+Si6O15) is reported in a peralkaline rhyolitic ignimbrite from the 11 island of Pantelleria, Italy. The mineral formed during devitrification of glassy fiamme and varies in form from anhedral plates to 12 perfect euhedral in open vesicles. There is significant replacement of Fe2+ by Mn (FMQ in the presence of a 14 hydrous fluid
A new, pre-Green Tuff (46 ka) volcanic stratigraphy is presented for the peralkaline Pantelleria Vol...
The island of Pantelleria consists of trachytes, pantellerites and minor mildly alkaline basalts. Ro...
In the last 50 ka basalts have erupted outside the margin of the young caldera on the island of Pan...
An occurrence of the rare mineral tuhualite (NaFe3+Fe2+Si6O15) is reported in a peralkaline rhyoliti...
Pantelleria island is the type locality for pantellerite, an iron and alkali-rich rhyolite. The erup...
The Green Tuff Ignimbrite, Pantelleria, is compositionally zoned from pantellerite at the base to co...
International audienceThe island of Pantelleria is one of the best known localities of bimodal mafic...
Trachyte and peralkaline rhyolite (pantellerite and comendite) frequently comprise the felsic end-me...
The island of Pantelleria is one of the best known localities of bimodal mafic-felsic magmatism (alk...
The eruptive history of Pantelleria has been marked by the eruption of nine peralkaline ignimbrites,...
International audiencePhase equilibrium experiments are recognized as an excellent method to determi...
The Green Tuff Ignimbrite, Pantelleria, is compositionally zoned from pantellerite at the base to co...
The recent (<190 ka) volcanic history of Pantelleria is characterized by the eruption of nine per...
Pantelleria Island is the type locality of pantellerite, an iron and alkali-rich rhyolite (P.I=mola...
The distribution and compositions of chevkinite-group minerals (CGMs) in the pantelleritic Gold Flat...
A new, pre-Green Tuff (46 ka) volcanic stratigraphy is presented for the peralkaline Pantelleria Vol...
The island of Pantelleria consists of trachytes, pantellerites and minor mildly alkaline basalts. Ro...
In the last 50 ka basalts have erupted outside the margin of the young caldera on the island of Pan...
An occurrence of the rare mineral tuhualite (NaFe3+Fe2+Si6O15) is reported in a peralkaline rhyoliti...
Pantelleria island is the type locality for pantellerite, an iron and alkali-rich rhyolite. The erup...
The Green Tuff Ignimbrite, Pantelleria, is compositionally zoned from pantellerite at the base to co...
International audienceThe island of Pantelleria is one of the best known localities of bimodal mafic...
Trachyte and peralkaline rhyolite (pantellerite and comendite) frequently comprise the felsic end-me...
The island of Pantelleria is one of the best known localities of bimodal mafic-felsic magmatism (alk...
The eruptive history of Pantelleria has been marked by the eruption of nine peralkaline ignimbrites,...
International audiencePhase equilibrium experiments are recognized as an excellent method to determi...
The Green Tuff Ignimbrite, Pantelleria, is compositionally zoned from pantellerite at the base to co...
The recent (<190 ka) volcanic history of Pantelleria is characterized by the eruption of nine per...
Pantelleria Island is the type locality of pantellerite, an iron and alkali-rich rhyolite (P.I=mola...
The distribution and compositions of chevkinite-group minerals (CGMs) in the pantelleritic Gold Flat...
A new, pre-Green Tuff (46 ka) volcanic stratigraphy is presented for the peralkaline Pantelleria Vol...
The island of Pantelleria consists of trachytes, pantellerites and minor mildly alkaline basalts. Ro...
In the last 50 ka basalts have erupted outside the margin of the young caldera on the island of Pan...