Citation: Jc. Tanguy et al., EVOLUTION OF THE MOUNT ETNA MAGMA - CONSTRAINTS ON THE PRESENT FEEDING SYSTEM AND ERUPTIVE MECHANISM, Journal of volcanology and geothermal research, 75(3-4), 1997, pp. 221-250
Citation: S. Rihs et al., U-SERIES AND TH-SERIES RADIONUCLIDES IN CO2-RICH GEOTHERMAL SYSTEMS IN THE FRENCH MASSIF-CENTRAL, Journal of radioanalytical and nuclear chemistry, 226(1-2), 1997, pp. 149-157
Citation: M. Condomines, DATING RECENT VOLCANIC-ROCKS THROUGH TH-230-U-238 DISEQUILIBRIUM IN ACCESSORY MINERALS - EXAMPLE OF THE PUY-DE-DOME (FRENCH MASSIF-CENTRAL), Geology, 25(4), 1997, pp. 375-378
Citation: M. Condomines et al., MAGMA DYNAMICS AT MT ETNA - CONSTRAINTS FROM U-TH-RA-PB RADIOACTIVE DISEQUILIBRIA AND SR ISOTOPES IN HISTORICAL LAVAS, Earth and planetary science letters, 132(1-4), 1995, pp. 25-41
Authors:
HEMOND C
HOFMANN AW
HEUSSER G
CONDOMINES M
RACZEK I
RHODES JM
Citation: C. Hemond et al., U-TH-RA SYSTEMATICS IN KILAUEA AND MAUNA-LOA BASALTS, HAWAII (VOL 116, PG 163, 1994), Chemical geology, 120(1-2), 1995, pp. 171-171
Citation: M. Condomines, THE VOLUME AND RESIDENCE TIME OF MAGMA BENEATH ACTIVE VOLCANOS DETERMINED BY DECAY SERIES DISEQUILIBRIA METHODS - COMMENT, Earth and planetary science letters, 122(1-2), 1994, pp. 251-255
Citation: M. Condomines et O. Sigmarsson, WHY ARE SO MANY ARC MAGMAS CLOSE TO U-238 TH-230 RADIOACTIVE EQUILIBRIUM, Geochimica et cosmochimica acta, 57(18), 1993, pp. 4491-4497