- 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...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1007/s00445-007-0176-8
-
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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
- Language:
- English
- Keywords:
- Copyright date:
- 2008
Journal article
Paleomagnetic evidence for low-temperature emplacement of the phreatomagmatic Peperino Albano ignimbrite (Colli Albani volcano, Central Italy)
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