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Paleomagnetic evidence for low-temperature emplacement of the phreatomagmatic Peperino Albano ignimbrite (Colli Albani volcano, Central Italy)

Abstract:

The Peperino Albano (approximately 19-36 ka old) is a phreatomagmatic pyroclastic flow deposit, cropping out along the slopes of the associated Albano maar (Colli Albani volcano, Italy). The deposit exhibits lateral and vertical transitions from valley pond to veneer facies, as well as intracrater facies. We present the results of a paleomagnetic study of thermal remanent magnetization (TRM) of the lithic clasts of the Peperino Albano ignimbrite that provide quantitative estimates of the rang...

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Publication status:
Published

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Publisher copy:
10.1007/s00445-007-0176-8

Authors


Porreca, M More by this author
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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Giordano, G More by this author
McClelland, E More by this author
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Journal:
BULLETIN OF VOLCANOLOGY
Volume:
70
Issue:
7
Pages:
877-893
Publication date:
2008-05-05
DOI:
EISSN:
1432-0819
ISSN:
0258-8900
URN:
uuid:38743cc3-2866-4282-9108-07c160199ff6
Source identifiers:
82073
Local pid:
pubs:82073

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