Using thermal remanent magnetisation (TRM) to distinguish block and ash flow and debris flow deposits, and to estimate their emplacement temperature: 1991–1995 lava dome eruption at Mt. Unzen Volcano, Japan

Author:

Uehara D.,Cas R.A.F.,Folkes C.,Takarada S.,Oda H.,Porreca M.

Funder

Monash University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

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2. Emplacement temperature determinations of proximal pyroclastic deposits on Santorini, Greece, and their implications;Bardot;Bull. Volcanol.,2000

3. The reliability of emplacement temperature estimates using palaeomagnetic methods: a case study from Santorini, Greece;Bardot;Geophys. J. Int.,2000

4. Emplacement temperatures of pyroclastic deposits on Santorini deduced from palaeomagnetic measurements: constraints on eruption mechanisms;Bardot;Geol. Soc. Lond., Spec. Publ.,1996

5. Emplacement Temperatures Determined by Progressive Thermal Demagnetisation Of Six Volcanic Deposits from the 1990–1995 Eruption of Unzen-Fugendake, Southwestern Japan, Cities on Volcanoes 5;Brenna,2007

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