IN PRIMO PIANO

(a) Global MOLA topography at 128 pixels per degree. (b) The structural mapping of this study overlaid on a MOLA-derived hillshade map

1 Agosto 2015

Self-similar clustering distribution of structural features...

Pozzobon R., F. Mazzarini, M. Massironi, ...

INGV Sezione di pisa - Seminari 2015

1 Agosto 2015

A detailed analysis of micro-seismicity induced...

| 2 settembre 2015 | ore ...

Sala sismica

31 Luglio 2015

Rinnovato il Protocollo d’Intesa tra INGV...

31 Luglio 2015 È stato rinnovato ...

Plagioclase size distributions of the 2001 Etnean products. The CSDs are summations for samples from each of the three eruptive vents. The increase in the total number of crystals increased the number of crystals that populate the largest size classes

23 Luglio 2015

Crystal size distributions of plagioclase in...

Fornaciai A., C. Perinelli, P. Armienti and M. Favalli ...

Fig. 4. Downflow output obtained on the western flank of Mt Etna from the subterminal vent opened at 3050 m above sea level in 2006 to the west of the Southeast Crater.

22 Luglio 2015

Simulating the area covered by lava...

Tarquini S., M. Favalli (2015). Geological ...

Photographs of comenditic trachyte enclaves from the Randazzo pumice cone and Khaggiar lava flow. (a): fresh‐cut surfaces of a block showing the porphyritic texture of the enclaves given by abundant large crystals of anorthoclase embedded in a gray matrix. Subspherical vesicles are dispersed in the enclaves. (b): the typical globular external margin of the enclaves. (c): block cut perpendicular to the surface showing undulate margins with deep indents (d): small enclaves (light gray with feldspar phenocrysts) dispersed in the Khaggiar lava. (e): enclaves in the Khaggiar lava characterized by a crenulated surface, porphyritic texture and subspherical vesicles

22 Luglio 2015

Cooling and crystallization recorded in trachytic...

Landi P., S.G. Rotolo. Journal of ...

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