References
Avedik F, Geli L (1987) Single channel seismic data from the East Pacific Rise axis between
11°504
0 N and 12°54
0 N. Geology 15:857–860
Ballard RD, Holcomb RT, van Andel TH (1979) The Galapagos Rift at 86°W: sheet flows,
collapsed pits, and lava lakes of the rift valley. J Geophys Res 84:5407–5422
Batiza R (1980) Origin and petrology of young oceanic central volcanoes: are most tholeiitic
rather than alkalic? Geology 8:477–483
Batiza R (1981) Quantitative data on the abundance and distribution of seamounts in the Pacific
Ocean. McDonnell Center for Space Sciences Pub. MCP-498, p 23
Batiza R, Fornari DJ, Vanko DA, Lonsdale P (1984) Craters, calderas, and hyaloclastites on
young Pacific seamounts. J Geophys Res 89:8371–8390
Bideau D, Hekinian R, Sichler B, Gracia E, Bollinger C, Constantin M, Guivel C (1998)
Contrasting volcanic-tectonic processes during the past 2 Ma on the Mid-Atlantic Ridge:
submersible mapping, petrological and magnetic results at latitude 34°52
0 N and 33°55
0 N. Mar
Geophys Res 20:425–458
Binard N, Hekinian R, Cheminee J-L, Searle C (1991) Morphological and structural studies of the
society and Austral hot spot regions in the South Pacific. Tectonophysics 186:293–312
Binard N, Hekinian R, Cheminée J-L, and Stoffers P (1992) Styles of eruptive activity on
intraplate volcanoes. J Geophys Res 97(13):999–14015
Bischoff JL, Pitzer KS (1989) Liquid-vapor relations for the system NaCl-H2O: summary of the
P-T-x surface from 300 °C to 500 °C. Am Jour Sci 289:217–248
Bischoff JL, Pitzer KS (1985) Phase relation and seafloor hydrothermal systems. Earth Planet Sci
lett 75:327–338
Blank JG, Brooker RA (1994) Experimental studies of carbon dioxide in silicate melt: solubility,
speciation and stable carbon isotope behavior. Rev Miner 30:157–186
Blong R (1984) Volcanic hazards. Academic Press, New York, p 424
Bonatti E, Harrison CG (1988) Eruption styles of basalt in oceanic spreading ridges and
seamounts: effects of magma temperature and viscosity. J Geophys Res 93:2967–2980
Bottinga Y, Javoy M (1989) MORB degassing evolutions of CO 2 . Earth Planet Sci Lett
95:215–225
Broecker WS (1985) How to build a habitable planet. ELDIGIO Press, New York
Burton MR, Mader HM, Polacci MM (2007) The role of gas percolation in quiescent degassing of
persistently active basaltic volcanoes. Earth Planet Sci Lett 264:46–60
Cayol V, Dieterich J. Okamura A, Miklius A (2000) High magma storage rates before the 1983
eruption of kilauea, Hawaii. Science, 288:2343–2346
Chaigneau M, Hekinian R, Cheminée J-L (1980) Magmatic gases extracted and analysed from
ocean floor volcanics. Bull Volcanl 43–1:241–253
Clague DA, Davis AS, Bischoff JL, Dixon JE, Geyer R (2000) Lava bubble formed by submarine
hydrovolcanic explosion on Lo’ihi Seamount and Kilauea Volcano. Bull Volcanol
61(7):437–449
Cromie WJ (1962) Earthquakes. Science services, vol 1. Nelson Doubleday Inc. Garden city, p 64
Cyamex Scientific Team (1978) Découverte par submersible de sulfures polymétalliques massifs
sur la dorsale du Pacifique oriental par 21°N (projet Rita). Compte Rendu Acad Sci Serie D,
287:1365–1368
Detrick RSP, Buhl P, Vern E, Mutter J, Orcutt J, Madsen J, Brocher T (1987) Multi-channel
imaging of a crustal magma chamber along the East Pacific Rise. Nature 326:35–41
Eissen P, Fouquet Y, Hardy D, and Ondréas H (2004) Recent MORB volcaniclastic explosive
deposits formed between 500 and 1750 m.b.s.l. on the axis of the Mid-Atlantic Ridge, south
of the Azores. Am Geophys Union Geophys Monogr 140. doi: 10.1020/140GM09
Fisher RV and Schmincke H-U, (1984) Pyroclastic rocks. Springer, Berlin, p 472
Fisher VR, Heiken K, Hulen JB (1998) Volcanoes; Crucible of change. Princeton University
Press, Princeton, p 317
References
141
Avedik F, Geli L (1987) Single channel seismic data from the East Pacific Rise axis between
11°504
0 N and 12°54
0 N. Geology 15:857–860
Ballard RD, Holcomb RT, van Andel TH (1979) The Galapagos Rift at 86°W: sheet flows,
collapsed pits, and lava lakes of the rift valley. J Geophys Res 84:5407–5422
Batiza R (1980) Origin and petrology of young oceanic central volcanoes: are most tholeiitic
rather than alkalic? Geology 8:477–483
Batiza R (1981) Quantitative data on the abundance and distribution of seamounts in the Pacific
Ocean. McDonnell Center for Space Sciences Pub. MCP-498, p 23
Batiza R, Fornari DJ, Vanko DA, Lonsdale P (1984) Craters, calderas, and hyaloclastites on
young Pacific seamounts. J Geophys Res 89:8371–8390
Bideau D, Hekinian R, Sichler B, Gracia E, Bollinger C, Constantin M, Guivel C (1998)
Contrasting volcanic-tectonic processes during the past 2 Ma on the Mid-Atlantic Ridge:
submersible mapping, petrological and magnetic results at latitude 34°52
0 N and 33°55
0 N. Mar
Geophys Res 20:425–458
Binard N, Hekinian R, Cheminee J-L, Searle C (1991) Morphological and structural studies of the
society and Austral hot spot regions in the South Pacific. Tectonophysics 186:293–312
Binard N, Hekinian R, Cheminée J-L, and Stoffers P (1992) Styles of eruptive activity on
intraplate volcanoes. J Geophys Res 97(13):999–14015
Bischoff JL, Pitzer KS (1989) Liquid-vapor relations for the system NaCl-H2O: summary of the
P-T-x surface from 300 °C to 500 °C. Am Jour Sci 289:217–248
Bischoff JL, Pitzer KS (1985) Phase relation and seafloor hydrothermal systems. Earth Planet Sci
lett 75:327–338
Blank JG, Brooker RA (1994) Experimental studies of carbon dioxide in silicate melt: solubility,
speciation and stable carbon isotope behavior. Rev Miner 30:157–186
Blong R (1984) Volcanic hazards. Academic Press, New York, p 424
Bonatti E, Harrison CG (1988) Eruption styles of basalt in oceanic spreading ridges and
seamounts: effects of magma temperature and viscosity. J Geophys Res 93:2967–2980
Bottinga Y, Javoy M (1989) MORB degassing evolutions of CO 2 . Earth Planet Sci Lett
95:215–225
Broecker WS (1985) How to build a habitable planet. ELDIGIO Press, New York
Burton MR, Mader HM, Polacci MM (2007) The role of gas percolation in quiescent degassing of
persistently active basaltic volcanoes. Earth Planet Sci Lett 264:46–60
Cayol V, Dieterich J. Okamura A, Miklius A (2000) High magma storage rates before the 1983
eruption of kilauea, Hawaii. Science, 288:2343–2346
Chaigneau M, Hekinian R, Cheminée J-L (1980) Magmatic gases extracted and analysed from
ocean floor volcanics. Bull Volcanl 43–1:241–253
Clague DA, Davis AS, Bischoff JL, Dixon JE, Geyer R (2000) Lava bubble formed by submarine
hydrovolcanic explosion on Lo’ihi Seamount and Kilauea Volcano. Bull Volcanol
61(7):437–449
Cromie WJ (1962) Earthquakes. Science services, vol 1. Nelson Doubleday Inc. Garden city, p 64
Cyamex Scientific Team (1978) Découverte par submersible de sulfures polymétalliques massifs
sur la dorsale du Pacifique oriental par 21°N (projet Rita). Compte Rendu Acad Sci Serie D,
287:1365–1368
Detrick RSP, Buhl P, Vern E, Mutter J, Orcutt J, Madsen J, Brocher T (1987) Multi-channel
imaging of a crustal magma chamber along the East Pacific Rise. Nature 326:35–41
Eissen P, Fouquet Y, Hardy D, and Ondréas H (2004) Recent MORB volcaniclastic explosive
deposits formed between 500 and 1750 m.b.s.l. on the axis of the Mid-Atlantic Ridge, south
of the Azores. Am Geophys Union Geophys Monogr 140. doi: 10.1020/140GM09
Fisher RV and Schmincke H-U, (1984) Pyroclastic rocks. Springer, Berlin, p 472
Fisher VR, Heiken K, Hulen JB (1998) Volcanoes; Crucible of change. Princeton University
Press, Princeton, p 317
References
141