G. D. Andrews and M. Branney, Emplacement and rheomorphic deformation of a large, 610 lava-like rhyolitic ignimbrite: Grey's Landing, southern Idaho, Bulletin, vol.123, pp.725-743, 2011.

C. Bonadonna and A. Costa, Estimating the volume of tephra deposits: A new simple strategy, Geology, vol.40, issue.5, pp.613-415, 2012.
DOI : 10.1130/G32769.1

M. J. Branney and P. Kokelaar, Pyroclastic density currents and the sedimentation of 615 ignimbrites, pp.152-616, 2002.

M. J. Branney, T. L. Barry, and M. Godchaux, Sheathfolds in rheomorphic ignimbrites, Bulletin of Volcanology, vol.66, issue.6, pp.485-491, 2004.
DOI : 10.1007/s00445-003-0332-8

L. Civetta, Y. Cornette, G. Crisci, P. Y. Gillot, G. Orsi et al., Geology, geochronology and chemical evolution of the island of Pantelleria, Geological Magazine, vol.32, issue.701, pp.541-562, 1984.
DOI : 10.1007/BF02596899

L. Civetta, Y. Cornette, G. Crisci, P. Y. Gillot, and G. Orsi, The eruptive history of Pantelleria (Sicily channel) in the last 50 ka, Bulletin of Volcanology, vol.6, issue.(1), pp.47-57, 1988.
DOI : 10.1007/BF01047508

D. Civile, E. Lodolo, L. Tortorici, G. Lanzafame, and G. Brancolini, Relationships between 624 magmatism and tectonics in a continental rift: the Pantelleria Island region (Sicily Channel, p.625, 2008.

D. Carlo, I. Rotolo, S. G. Scaillet, B. Buccheri, V. Pichavant et al., Phase Equilibrium Constraints on Pre-eruptive Conditions of Recent Felsic Explosive Volcanism at Pantelleria Island, Italy, Journal of Petrology, vol.51, issue.11, pp.2245-2276, 2010.
DOI : 10.1093/petrology/egq055
URL : https://hal.archives-ouvertes.fr/insu-00556917

A. Gioncada and P. Landi, The pre-eruptive volatile contents of recent basaltic and 635 pantelleritic magmas at Pantelleria (Italy), Journal of Volcanology and Geothermal Research, vol.636, pp.189-191, 2010.

L. Felice and S. , Tephrostratigraphy of silicic volcanism at Pantelleria island, combining field 638 observations, petrochemical data and 40 Ar/ 39 Ar dating: implications on magmatic system, p.640, 2008.

P. W. Lipman, The roots of ash flow calderas in western North America: Windows into the tops of granitic batholiths, Journal of Geophysical Research, vol.89, issue.B10, pp.8801-8841, 1984.
DOI : 10.1029/JB089iB10p08801

R. Macdonald, Nomenclature and petrochemistry of the peralkaline oversaturated extrusive rocks, Bulletin Volcanologique, vol.38, issue.2, pp.498-505, 1974.
DOI : 10.1007/BF02596896

G. A. Mahood, Pyroclastic rocks and calderas associated with strongly peralkaline magmatism, Journal of Geophysical Research, vol.45, issue.108, pp.8540-8552, 1984.
DOI : 10.1029/JB089iB10p08540

G. A. Mahood and W. Hildreth, Nested calderas and trapdoor uplift at Pantelleria, Strait of 647 Sicily, Geology, vol.11, pp.103-106, 1983.

M. Mattia, A. Bonnacorso, and F. Guglielmino, Ground deformations in the island of 651, 2007.

D. A. Neave, G. Fabbro, R. A. Herd, C. M. Petrone, and M. Edmonds, Melting, Differentiation and Degassing at the Pantelleria Volcano, Italy, 2012. Melting, differentiation 654 and degassing at the Pantelleria volcano, pp.637-663
DOI : 10.1093/petrology/egr074

F. A. Ochs and R. A. Lanhe, The Density of Hydrous Magmatic Liquids, Science, vol.283, issue.5406, pp.1314-1317, 1999.
DOI : 10.1126/science.283.5406.1314

S. L. Quane and J. K. Russell, Ranking welding intensity in pyroclastic deposits, Bulletin of Volcanology, vol.9, issue.2, pp.129-143, 2005.
DOI : 10.1007/s00445-004-0367-5

N. Romengo, Relationships between mafic and felsic magmatism at Pantelleria: a 660 petrological study on intermediate trachyte magmas, p.661, 2011.

S. G. Rotolo, F. Castorina, D. Cellura, and M. Pompilio, Petrology and Geochemistry of Submarine Volcanism in the Sicily Channel Rift, The Journal of Geology, vol.114, issue.3, pp.355-365, 2006.
DOI : 10.1086/501223

S. G. Rotolo, L. Felice, S. Mangalaviti, A. Landi, and P. , Geology and petrochemistry of the 664 recent (< 25 ka) silicic volcanism at Pantelleria island, Bollettino Società Geologica Italiana, vol.665, pp.126-191, 2007.

S. Scaillet, G. Vita-scaillet, and H. Guillou, Oldest human footprints dated by Ar/Ar, Earth and Planetary Science Letters, vol.275, issue.3-4, pp.320-325, 2008.
DOI : 10.1016/j.epsl.2008.08.026

S. Scaillet, S. G. Rotolo, L. Felice, S. Vita, and G. , High-resolution 40 Ar/ 39 Ar 669 chronostratigraphy of the post-caldera (< 20 ka) volcanic activity at Pantelleria, Sicily Strait, Earth and Planetary Science Letters, vol.670, issue.309, 2011.

F. Speranza, P. Landi, F. D-'ajello-caracciolo, and A. Pignatelli, Paleomagnetic dating of the 672 most recent silicic eruptive activity at Pantelleria (Strait of Sicily), Bulletin of Volcanology, vol.673, pp.72-847, 2010.

F. Speranza, D. Chiara, A. Rotolo, and S. G. , Correlation of welded ignimbrites on Pantelleria (Strait of Sicily) using paleomagnetism, Bulletin of Volcanology, vol.108, issue.B10, pp.341-357, 2012.
DOI : 10.1007/s00445-011-0521-9

J. M. Sumner and M. J. Branney, The emplacement history of a remarkable heterogeneous, chemically zoned, rheomorphic and locally lava-like ignimbrite: ???TL??? on Gran Canaria, Journal of Volcanology and Geothermal Research, vol.115, issue.1-2, pp.109-138, 2002.
DOI : 10.1016/S0377-0273(01)00311-0

G. P. Walker, Ignimbrite types and ignimbrite problems, Journal of Volcanology and 681 Geothermal Research, pp.65-88, 1983.
DOI : 10.1016/0377-0273(83)90062-8

J. C. White, D. F. Parker, and M. Ren, The origin of trachytes and pantellerite from Pantelleria, p.683, 2009.

. Italy, Insights from major element, trace element and thermodynamic modelling, Journal of 684 Volcanology and Geothermal Research, vol.179, pp.33-55

J. A. Wolff and J. V. Wright, Formation of the Green Tuff, Pantelleria. Bulletin of Volcanology, vol.686, pp.44-681, 1981.

J. V. Wright, Stratigraphy and geology of the welded air-fall tuffs of Pantelleria, Italy, Geologische Rundschau, vol.12, issue.1, p.688, 1980.
DOI : 10.1007/BF01869037

. Zinedi, the lower portion of the section being covered by talus The sequence starts with Unit 868 P, here deeply weathered, for an exposed thickness > 5 m (the base is not visible) As 869 commonly observed elsewhere, P is crystal-rich (35-40 volume per cent) with alkali feldspar 870 phenocryst up to 10 mm, p.871

. Above, 50 cm thick, rich in lithics and loose crystals. Above, the 873 transition to Unit Z is sharp As a whole, unit Z (as thick as 6 m) is crystal-poor (! 20 874 volume per cent), with alkali feldspar up to 3 mm in size. The basal member is rich in streaky 875 fiamme and is followed by a lithic-rich layer (1 m thick, with rounded lithics up to 15 cm in 876 length) In this location, Z is characterized by a peculiar sawtooth erosional profile due to 877 alternating prominent glass-rich layers (2-10 cm thick the each) with more eroded fines-rich 878 levels (10-30 cm the each) The upper portion of Z (1 m thick) is distinctly lithic-rich, p.880

H. Mahood, 5 cm); the upper portion is rather massive, altough a crude lamination can 899 be distinguished, due principally to the strong sea water alteration that preferentially eroded 900 glass-rich layers. Phenocryst content is ! 20 volume per cent, with alkali feldspar ! 3-5 mm in 901 length. Lithics are abundant and small (2-5 cm) in the lower half, mostly consisting of 902 holocrystalline microsyenites. The upper half of the unit is less lithic rich and shows distinct 903 rheomorphic folding. 904 The sequence is topped by the Green Tuff, up to 4 m thick, that starts with a basal 905 vitrophyre 5-15 cm thick and continues with the main ignimbrite body without any clear 906 internal structure, pp.908-914, 1986.