@article {Fornari2012,
	title = {{The East Pacific Rise Between 9 degrees N and 10 degrees N: Twenty-Five Years of Integrated, Multidisciplinary Oceanic Spreading Center Studies}},
	journal = {Oceanography},
	volume = {25},
	number = {1},
	year = {2012},
	month = {mar},
	pages = {18{\textendash}43},
	publisher = {OCEANOGRAPHY SOC},
	address = {ROCKVILLE; P.O. BOX 1931, ROCKVILLE, MD USA},
	abstract = {The East Pacific Rise from {\~{}}~9{\textendash}10{\textdegree}N is an archetype for a fast-spreading mid-ocean ridge. In particular, the segment near 9{\textdegree}50{\textquoteright}N has been the focus of multidisciplinary research for over two decades, making it one of the best-studied areas of the global ridge system. It is also one of only two sites along the global ridge where two historical volcanic eruptions have been observed. This volcanically active segment has thus offered unparalleled opportunities to investigate a range of complex interactions among magmatic, volcanic, hydrothermal, and biological processes associated with crustal accretion over a full magmatic cycle. At this 9{\textdegree}50{\textquoteright}N site, comprehensive physical oceanographic measurements and modeling have also shed light on linkages between hydrodynamic transport of larvae and other materials and biological dynamics influenced by magmatic processes. Integrated results of high-resolution mapping, and both in~situ and laboratory-based geophysical, oceanographic, geochemical, and biological observations and sampling, reveal how magmatic events perturb the hydrothermal system and the biological communities it hosts.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2012.02},
	author = {Fornari, D J and Von Damm, K L and Bryce, Julia G and Cowen, J P and Ferrini, Vicki and Fundis, A and Lilley, M D and Luther, G W and Mullineaux, L S and Perfit, M R and Meana-Prado, M F and Rubin, K H and Seyfried, W E and Shank, T M and Soule, S A and Tolstoy, M and White, S M}
}
@article {Colman2012,
	title = {{Effects of variable magma supply on mid-ocean ridge eruptions: Constraints from mapped lava flow fields along the Gal{\'a}pagos Spreading Center}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {13},
	number = {8},
	year = {2012},
	pages = {Q08014},
	abstract = {Mapping and sampling of 18 eruptive units in two study areas along the Gal{\'a}pagos Spreading Center (GSC) provide insight into how magma supply affects mid-ocean ridge (MOR) volcanic eruptions. The two study areas have similar spreading rates (53 versus 55~mm/yr), but differ by 30{\%} in the time-averaged rate of magma supply (0.3~{\texttimes}~106 versus 0.4~{\texttimes}~106~m3/yr/km). Detailed geologic maps of each study area incorporate observations of flow contacts and sediment thickness, in addition to sample petrology, geomagnetic paleointensity, and inferences from high-resolution bathymetry data. At the lower-magma-supply study area, eruptions typically produce irregularly shaped clusters of pillow mounds with total eruptive volumes ranging from 0.09 to 1.3~km3. At the higher-magma-supply study area, lava morphologies characteristic of higher effusion rates are more common, eruptions typically occur along elongated fissures, and eruptive volumes are an order of magnitude smaller (0.002{\textendash}0.13~km3). At this site, glass MgO contents (2.7{\textendash}8.4 wt. {\%}) and corresponding liquidus temperatures are lower on average, and more variable, than those at the lower-magma-supply study area (6.2{\textendash}9.1 wt. {\%} MgO). The differences in eruptive volume, lava temperature, morphology, and inferred eruption rates observed between the two areas along the GSC are similar to those that have previously been related to variable spreading rates on the global MOR system. Importantly, the documentation of multiple sequences of eruptions at each study area, representing hundreds to thousands of years, provides constraints on the variability in eruptive style at a given magma supply and spreading rate.},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2012GC004163},
	url = {http://dx.doi.org/10.1029/2012GC004163},
	author = {Colman, A and Sinton, J M and White, S M and McClinton, J T and Bowles, J A and Rubin, K H and Behn, M D and Cushman, B and Eason, D E and Gregg, T K P and Gr{\"o}nvold, Karl and Hidalgo, S and Howell, J and Neill, O and Russo, Chris}
}
@article {White2002,
	title = {{Correlation between volcanic and tectonic segmentation of fast-spreading ridges: Evidence from volcanic structures and lava flow morphology on the East Pacific Rise at 9 degrees -10 degrees N}},
	journal = {Journal of Geophysical Research},
	volume = {107},
	number = {B8},
	year = {2002},
	pages = {Article no. 2173},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2001JB000571},
	url = {http://dx.doi.org/10.1029/2001JB000571},
	author = {White, S M and Haymon, R M and Fornari, D J and Macdonald, K C and Perfit, M R}
}
@article {Sinton2002,
	title = {{Volcanic eruptions on mid-ocean ridges: New evidence from the superfast spreading East Pacific Rise, 17 degrees-19 degrees S}},
	journal = {Journal of Geophysical Research},
	volume = {107},
	number = {B6},
	year = {2002},
	pages = {Article no. 2115},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2000JB000090},
	url = {http://dx.doi.org/10.1029/2000JB000090},
	author = {Sinton, J and Bergmanis, E and Rubin, K H and Batiza, R and Gregg, T K P and Gronvold, K and Macdonald, K C and White, S M}
}
