Gas transport model for the magmatic system at Mount Pinatubo, Philippines: Insights from (210Pb)/(226Ra)

Journal of Volcanology and Geothermal Research

Volumn 181, Issue 1-2, 2009, Pages 124-140

  Kayzar, Theresa M ^a   Cooper, Kari M ^b   Reagan, Mark K ^c   Kent, Adam J R ^d  

^a UNIVERSITY OF WASHINGTON   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

^c UNIVERSITY OF IOWA   (United States)

^d OREGON STATE UNIVERSITY   (United States)

Author keywords

degassing; Pb 210; Pinatubo; Ra 226; timescales

Indexed keywords

ACTINIDES; BASALT; DEGASSING; GASES; LEAD; MINERALS; MOUNTINGS; RADON; TRACE ELEMENTS; TRANSURANIUM ELEMENTS; URANIUM; VOLCANOES;

BASALTIC MAGMAS; BASALTIC MELTS; BUBBLE PLUMES; CONCEPTUAL MODELS; CRYSTAL MATRICES; DACITE MAGMAS; GAS ACCUMULATIONS; GAS MOTIONS; GAS TRANSPORTS; GAS-PHASE; LOW VISCOSITIES; MAGMATIC SOURCES; MAGMATIC SYSTEMS; PB-210; PHILIPPINES; PINATUBO; QUANTITATIVE INVESTIGATIONS; RA-226; ROCK SAMPLES; TIME SEQUENCES; TIME-SCALE; TIMESCALES;

LEAD ALLOYS;

DACITE; DEGASSING; GAS TRANSPORT; LAVA DOME; LEAD ISOTOPE; MAGMATISM; MANTLE PLUME; NUMERICAL MODEL; RADIUM ISOTOPE; TEPHRA; TEPHROCHRONOLOGY; TIMESCALE; VENTING; VOLCANIC ERUPTION; VOLCANOLOGY;

ASIA; CENTRAL LUZON; EURASIA; LUZON; MOUNT PINATUBO; PHILIPPINES; SOUTHEAST ASIA; ZAMBALES;

PINATUBO;

EID: 60749085314     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.01.006     Document Type: Article

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