Charcoal reflectance as a proxy for the emplacement temperature of pyroclastic flow deposits
- 1 January 2005
- journal article
- Published by Geological Society of America in Geology
- Vol. 33 (7) , 589
- https://doi.org/10.1130/g21474.1
Abstract
No abstract availableThis publication has 13 references indexed in Scilit:
- Palaeotemperature determinations for the 1.8-ka Taupo ignimbrite, New Zealand, and implications for the emplacement history of a high-velocity pyroclastic flowBulletin of Volcanology, 2004
- Herculaneum victims of Vesuvius in ad 79Nature, 2001
- Mobility of pyroclastic flows and surges at the Soufriere Hills Volcano, MontserratGeophysical Research Letters, 1999
- Abrupt changes (jumps) in reflectance values and chemical compositions of artificial charcoals and inertinite in coalsInternational Journal of Coal Geology, 1999
- Pyroclastic flows generated by gravitational instability of the 1996–97 Lava Dome of Soufriere Hills Volcano, MontserratGeophysical Research Letters, 1998
- FTIR spectroscopy and reflectance of modern charcoals and fungal decayed woods: implications for studies of inertinite in coalsInternational Journal of Coal Geology, 1998
- Cooling, degassing and compaction of rhyolitic ash flow tuffs: a computational modelBulletin of Volcanology, 1995
- Palaeomagnetic estimates of emplacement temperatures of pyroclastic deposits on Santorini, GreeceBulletin of Volcanology, 1989
- Palaeomagnetic determination of emplacement temperature of Vesuvius AD 79 pyroclastic depositsNature, 1981
- Application de la spectrometrie infrarouge a l'etude des bois fossilises dans les formations volcaniquesBSGF - Earth Sciences Bulletin, 1971