Crystallization conditions of leucite-bearing magmas and their implications on the magmatological evolution of ultrapotassic magmas: the Vico Volcano, Central Italy

2002 ◽  
Vol 74 (2-4) ◽  
pp. 253-276 ◽  
Author(s):  
G. Perini ◽  
S. Conticelli
2000 ◽  
Vol 95 (1-4) ◽  
pp. 247-272 ◽  
Author(s):  
Giulia Perini ◽  
Sandro Conticelli ◽  
Lorella Francalanci ◽  
Jon P. Davidson

2020 ◽  
Vol 243 ◽  
pp. 106470
Author(s):  
Alison Pereira ◽  
Lorenzo Monaco ◽  
Fabrizio Marra ◽  
Sébastien Nomade ◽  
Mario Gaeta ◽  
...  

2001 ◽  
Vol 65 (6) ◽  
pp. 787-795 ◽  
Author(s):  
M. Gaeta ◽  
C. Freda

AbstractA magmatic calcic amphibole (M4Ca≥1.50) characterized by large Sr and F contents (SrO>1 wt.%, F>2.5 wt.%) is described. According to the crystal-chemical formula, the amphibole can be classified as a strontian fluoro-magnesiohastingsite and the presence of Sr cations in the A sites is suggested. The amphibole occurs in the groundmass of ultrapotassic lavas from the Alban Hills Volcanic District (Central Italy). This peculiar chemical composition is due to the lavas' groundmass compositional trend occurring under low silica-activity conditions. We suggest that the occurrence of F amphiboles allows us to consider the Alban Hills Volcanic District magmas to be as rich in F as other ultrapotassic magmas.


Agronomie ◽  
2001 ◽  
Vol 21 (3) ◽  
pp. 267-276
Author(s):  
Daniela Businelli ◽  
Enrico Tombesi ◽  
Marco Trevisan

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