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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7869

Authors: Speranza, F.*
Di Chiara, A.*
Rotolo, S. G.*
Title: Correlation of welded ignimbrites on Pantelleria (Strait of Sicily) using paleomagnetism
Title of journal: Bulletin of volcanology
Series/Report no.: 2/74 (2012)
Publisher: Springer Berlin Heidelberg
Issue Date: Mar-2012
DOI: 10.1007/s00445-011-0521-9
Keywords: Pantelleria
Ignimbrite
Caldera formation
Paleomagnetism
Paleosecular variation of the geomagnetic field
Abstract: Although the oldest volcanic rocks exposed at Pantelleria (Strait of Sicily) are older than 300 ka, most of the island is covered by the 45–50 ka Green Tuff ignimbrite, thought to be related to the Cinque Denti caldera, and younger lavas and scoria cones. Pre-50 ka rocks (predominantly rheomorphic ignimbrites) are exposed at isolated sea cliffs, and their stratigraphy and chronology are not completely resolved. Based on volcanic stratigraphy and K/Ar dating, it has been proposed that the older La Vecchia caldera is related to ignimbrite Q (114 ka), and that ignimbrites F, D, and Z (106, 94, and 79 ka, respectively) were erupted after caldera formation. We report here the paleomagnetic directions obtained from 23 sites in ignimbrite P (133 ka) and four younger ignimbrites, and from an uncorrelated (and loosely dated) welded lithic breccia thought to record a caldera-forming eruption. The paleosecular variation of the geomagnetic field recorded by ignimbrites is used as correlative tool, with an estimated time resolution in the order of 100 years. We find that ignimbrites D and Z correspond, in good agreement with recent Ar/Ar ages constraining the D/Z eruption to 87 ka. The welded lithic breccia correlates with a thinner breccia lying just below ignimbrite P at another locality, implying that collapse of the La Vecchia caldera took place at ~130–160 ka. This caldera was subsequently buried by ignimbrites P, Q, F, and D/Z. Paleomagnetic data also show that the northern caldera margin underwent a ~10° west–northwest (outwards) tilting after emplacement of ignimbrite P, possibly recording magma resurgence in the crust.
Appears in Collections:Papers Published / Papers in press
04.04.99. General or miscellaneous
04.04.08. Sediments: dating, processes, transport
04.04.10. Stratigraphy
04.04.11. Instruments and techniques
04.05.99. General or miscellaneous
04.05.02. Geomagnetic field variations and reversals
04.05.03. Global and regional models
04.05.06. Paleomagnetism
04.05.07. Rock magnetism
04.05.08. Instruments and techniques

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