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 lat. 34°52
0 N and 33°55
0 N. Marine
Geophys Res 20:425–458
Choukroune P, Francheteau J, Hekinian R (1984) Tectonics of the East Pacific Rise near 13°N
from field observations. Earth Planet Sci Lett 68:115–127
Cormier M-H, Scheirer DS, Macdonald KC (1996) Evolution of the East Pacific Rise at 17-198S
since 5 Ma: splitting of rapid migration of axial discontinuities. Marine Geophys Res
18:53–84
Coogan LA, Gillis KM, MacLeod CJ, Thompson JM, Hekinian R (2002) Petrology and
geochemistry of lower crust formed at the East Pacific rise and exposed at Hess Deep: a
synthesis and new results. Electronic J Earth Sci, Geochem Geophys Geosyst G3, Am
Geophys Union 3(11):1–30
DeMets C, Gordon RG, Argus DF, Stein S (1990) Current plate motions. Geophys Int
101:425–478
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
Detrick RS, Needham HD, Renard V (1995) Gravity anomalies and crustal thickness variation
along the Mid-Atlantic ridge between 13°N and 14°N. J Gephys Res 100:3767–3787
Eissen JP, Bideau D, Juteau T (1981) Présence de basalts porphyritiques dans les zones de
fractures de la dorsale Est-Pacifique. Compte Rendu Acad Sc Paris 293:61–66
Etienne J-L (2005) Clipperton- l’Atoll du bout du monde. Edition Septième continent, PAO
Editions du Seuil Normandie ROTO Impression SAS Lonrain, France, p 208
Février M (1981) Hydrothermalism and mineralisations sur la dorsale Est Pacifique à 21°N. PhD
Thesis, Université de Bretagne Occidentale, Troisième cycle : Structure et évolution
géologique des Océans, p 270
Flueh ER, Michael J, Fisher A, Bialas J, Childs JR, Klaeschen D, Kukowski N, Parsons T, Scholl
DW, Brink U, Trehu A-M, Vidal N (1998) New seismic images of the Cascadia subduction
zone from Cruise SO108 ORWELL. Tectonophysics 293:69–84
Fouquet Y, Knott R, Cambon P, Fallick A, Rickard D, Desbruyeres D (1996) Formation of large
sulfide mineral deposits along fast spreading ridges. Example from off-axial deposits at
12°43
0 N on the East Pacific Rise. Earth Planet Sci Lett 144(1):147–162
Francheteau J, Armijo R, Cheminée J-L, Hekinian R, Lonsdale P, Blum N (1992) Dyke complex
of the East Pacific Rise exposed in the walls of Hess Deep and the structure of the upper
oceanic crust. Earth Planet Sci Lett 111:109–121
Francheteau J, Ballard RD (1983) The East Pacific Rise near 21° N, 13°N and 20°S—inferences
for along-strike variability of axial processes of the mid-ocean ridge. Earth Planet Sci Lett
64:93–116
Francis TJG (1985) Resistivity measurements of an ocean sulfide deposit from the submersible
Cyana. Marine Geophys Res 7(3):419–437
Fujioka K, Massoth G, de Ronde C, Tanaka-Nakano A, Gendron J, Kinoshita M, Nishizawa A,
Okano O, Paradis G, Row K, Shinohara M, Shitashima K, Tsunogai U, Ytow N (1995) Active
hydrothermal systems of a super-fast spreading ridge, Southern East Pacific Rise (13°58
0 S to
18°26
0 S). InterRidge News 4:7–10
Gillis KM, Mével C, Allan J, Leg 147 Scientific Party (1993) Hydrothermal evolution of EPR
lower crust exposed at the Hess Deep. EOS, Trans Am Geophys Union 74(Suppl.):653
(Abstract)
Gracia E, Parson M, Bideau D, Hekinian R (1998) Volcano-tectonic variability along segments of
Mid-Atlantic ridge between the Azores platform and Hayes fracture zone: evidence from
submersible and high-resolution sidescan sonar data. In: Mills R, Harrison K (eds) Modern
ocean floor processes and the geological record, vol 148. Geological Society, Special
Publications, London, pp 1–15
Haymon RM (1996) The response of ridge crest hydrothermal system to segmented, episodic
magma supply. In: MacLeod CJ, Tyler PA, Walker CL (eds) Tectonic magmatic,
References
251
Contrasting volcanic-tectonic processes during the past 2 Ma on the Mid-Atlantic Ridge:
submersible mapping, petrological and magnetic results at lat. 34°52
0 N and 33°55
0 N. Marine
Geophys Res 20:425–458
Choukroune P, Francheteau J, Hekinian R (1984) Tectonics of the East Pacific Rise near 13°N
from field observations. Earth Planet Sci Lett 68:115–127
Cormier M-H, Scheirer DS, Macdonald KC (1996) Evolution of the East Pacific Rise at 17-198S
since 5 Ma: splitting of rapid migration of axial discontinuities. Marine Geophys Res
18:53–84
Coogan LA, Gillis KM, MacLeod CJ, Thompson JM, Hekinian R (2002) Petrology and
geochemistry of lower crust formed at the East Pacific rise and exposed at Hess Deep: a
synthesis and new results. Electronic J Earth Sci, Geochem Geophys Geosyst G3, Am
Geophys Union 3(11):1–30
DeMets C, Gordon RG, Argus DF, Stein S (1990) Current plate motions. Geophys Int
101:425–478
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
Detrick RS, Needham HD, Renard V (1995) Gravity anomalies and crustal thickness variation
along the Mid-Atlantic ridge between 13°N and 14°N. J Gephys Res 100:3767–3787
Eissen JP, Bideau D, Juteau T (1981) Présence de basalts porphyritiques dans les zones de
fractures de la dorsale Est-Pacifique. Compte Rendu Acad Sc Paris 293:61–66
Etienne J-L (2005) Clipperton- l’Atoll du bout du monde. Edition Septième continent, PAO
Editions du Seuil Normandie ROTO Impression SAS Lonrain, France, p 208
Février M (1981) Hydrothermalism and mineralisations sur la dorsale Est Pacifique à 21°N. PhD
Thesis, Université de Bretagne Occidentale, Troisième cycle : Structure et évolution
géologique des Océans, p 270
Flueh ER, Michael J, Fisher A, Bialas J, Childs JR, Klaeschen D, Kukowski N, Parsons T, Scholl
DW, Brink U, Trehu A-M, Vidal N (1998) New seismic images of the Cascadia subduction
zone from Cruise SO108 ORWELL. Tectonophysics 293:69–84
Fouquet Y, Knott R, Cambon P, Fallick A, Rickard D, Desbruyeres D (1996) Formation of large
sulfide mineral deposits along fast spreading ridges. Example from off-axial deposits at
12°43
0 N on the East Pacific Rise. Earth Planet Sci Lett 144(1):147–162
Francheteau J, Armijo R, Cheminée J-L, Hekinian R, Lonsdale P, Blum N (1992) Dyke complex
of the East Pacific Rise exposed in the walls of Hess Deep and the structure of the upper
oceanic crust. Earth Planet Sci Lett 111:109–121
Francheteau J, Ballard RD (1983) The East Pacific Rise near 21° N, 13°N and 20°S—inferences
for along-strike variability of axial processes of the mid-ocean ridge. Earth Planet Sci Lett
64:93–116
Francis TJG (1985) Resistivity measurements of an ocean sulfide deposit from the submersible
Cyana. Marine Geophys Res 7(3):419–437
Fujioka K, Massoth G, de Ronde C, Tanaka-Nakano A, Gendron J, Kinoshita M, Nishizawa A,
Okano O, Paradis G, Row K, Shinohara M, Shitashima K, Tsunogai U, Ytow N (1995) Active
hydrothermal systems of a super-fast spreading ridge, Southern East Pacific Rise (13°58
0 S to
18°26
0 S). InterRidge News 4:7–10
Gillis KM, Mével C, Allan J, Leg 147 Scientific Party (1993) Hydrothermal evolution of EPR
lower crust exposed at the Hess Deep. EOS, Trans Am Geophys Union 74(Suppl.):653
(Abstract)
Gracia E, Parson M, Bideau D, Hekinian R (1998) Volcano-tectonic variability along segments of
Mid-Atlantic ridge between the Azores platform and Hayes fracture zone: evidence from
submersible and high-resolution sidescan sonar data. In: Mills R, Harrison K (eds) Modern
ocean floor processes and the geological record, vol 148. Geological Society, Special
Publications, London, pp 1–15
Haymon RM (1996) The response of ridge crest hydrothermal system to segmented, episodic
magma supply. In: MacLeod CJ, Tyler PA, Walker CL (eds) Tectonic magmatic,
References
251