The volume and residence time of magma beneath active volcanoes determined by decay-series disequilibria methods

Author:

Pyle David M.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference47 articles.

1. The Usu-san eruption and the earthquake and elevation phenomena;Omori;Bull. Imp. Earthquake Inv. Comm. Tokyo,1913

2. Ground surface movement at Kilauea volcano;Wilson;Hawaii Univ. Hawaii Res. Publ.,1935

3. Relation between the eruptions of various volcanoes and the defromation of the ground surface around them;Mogi;Bull. Earthquake Res. Inst. Tokyo,1958

4. Modeling the three-dimensional structure of macroscopic magma transport systems: application to Kilauea volcano;Ryan;Hawaii J. Geophys. Res.,1981

5. Volcano tremor at Mount Etna: a brief description;Schick;Mem. Soc. Geol. Ital.,1982

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