Anatomy of a basaltic volcano

Nature ◽  
1993 ◽  
Vol 363 (6425) ◽  
pp. 125-133 ◽  
Author(s):  
Robert I. Tilling ◽  
John J. Dvorak
Keyword(s):  
Basaltic Volcano

scholarly journals Geomechanical rock properties of a basaltic volcano

2015 ◽  
Vol 3 ◽  
Author(s):  
Lauren N. Schaefer ◽  
Jackie E. Kendrick ◽  
Thomas Oommen ◽  
Yan Lavallée ◽  
Gustavo Chigna
Keyword(s):  
Rock Properties ◽  
Basaltic Volcano

scholarly journals Evidence of sheared sills related to flank destabilization in a basaltic volcano

2016 ◽  
Vol 674 ◽  
pp. 195-209 ◽  
Author(s):  
C. Berthod ◽  
V. Famin ◽  
J. Bascou ◽  
L. Michon ◽  
B. Ildefonse ◽  
...  
Keyword(s):  
Basaltic Volcano

Atmospheric sources and sinks of volcanogenic elements in a basaltic volcano (Etna, Italy)

2011 ◽  
Vol 75 (23) ◽  
pp. 7401-7425 ◽  
Author(s):  
S. Calabrese ◽  
A. Aiuppa ◽  
P. Allard ◽  
E. Bagnato ◽  
S. Bellomo ◽  
...  
Keyword(s):  
Sources And Sinks ◽  
Basaltic Volcano

Le 'volcan' de Beaulieu, pres Rognes (Bouches-du-Rhone)

1964 ◽  
Vol S7-VI (4) ◽  
pp. 443-455 ◽  
Author(s):  
Simonne Gueirard
Keyword(s):  
Olivine Basalt ◽  
Southern France ◽  
Basaltic Volcano ◽  
Lower Tertiary ◽  
Volcanic Conduit

Abstract The lower Tertiary Beaulieu basaltic volcano near Rognes in southern France had two episodes of activity, emitting pre-Stampian (pre-middle Oligocene) olivine basalt with lherzolite nodules, and a terminal upper Stampian (terminal middle Oligocene) dolerite flow with a pegmatoid facies. An upper Stampian conglomerate including volcanic fragments and also lenticular limestones lies between the flows. Terminal upper Stampian marl and limestone overlie the dolerite. The volcanic conduit probably lies at the intersection of a cross fault with one of the major northwest-trending faults characterizing the region.

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