@article {Greene2015,
	title = {{Geologic implications of seafloor character and carbonate lithification imaged on the domal core of Atlantis Massif}},
	journal = {Deep-Sea Research Part II: Topical Studies in Oceanography},
	volume = {121},
	year = {2015},
	pages = {246{\textendash}255},
	abstract = {We document the seafloor character on Atlantis Massif, an ocean core complex located at 30{\textdegree}N on the Mid-Atlantic Ridge, with an emphasis on the distribution of carbonate features. Seafloor imagery, near-bottom backscatter, and bathymetry were analyzed on the Central Dome and the Western Shoulder of the exposed footwall to the detachment, and on the Eastern Block, a hanging wall to the fault. We merged Argo II still images to produce photo-mosaics and evaluated these together with video imagery, acoustic reflectivity, and basic rock composition. The seafloor was classified as unconsolidated sediment, lithified carbonate crust, consolidated carbonate cap, exposed basement, or rubble, and the spatial distribution of each type was assessed. Unconsolidated sediment, exposed basement, and rubble were documented in all three regions studied. Lithified carbonate crust was also present on the Western Shoulder and eastern Central Dome. Consolidated carbonate cap was found on the Eastern Block. The formation of the carbonate rock is interpreted to reflect precipitation and/or sediment cementation via fluids derived from serpentinization. Both processes occur at the nearby Lost City Hydrothermal Field. The newly documented locations of seafloor carbonate lithification therefore mark pathways of past, possibly recent, fluid flux from subsurface water-rock reaction zones and represent an additional constituent of the carbon cycling hosted by oceanic lithosphere.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	doi = {10.1016/j.dsr2.2015.06.020},
	author = {Greene, J A and Tominaga, M and Blackman, D K}
}
@article {Blackman2011,
	title = {{Drilling constraints on lithospheric accretion and evolution at Atlantis Massif, Mid-Atlantic Ridge 30 degrees N}},
	journal = {Journal of Geophysical Research: Solid Earth},
	volume = {116},
	year = {2011},
	month = {jul},
	pages = {B07103{\textendash}B07103},
	publisher = {AMER GEOPHYSICAL UNION},
	address = {WASHINGTON; 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA},
	abstract = {Expeditions 304 and 305 of the Integrated Ocean Drilling Program cored and logged a 1.4 km section of the domal core of Atlantis Massif. Postdrilling research results summarized here constrain the structure and lithology of the Central Dome of this oceanic core complex. The dominantly gabbroic sequence recovered contrasts with predrilling predictions; application of the ground truth in subsequent geophysical processing has produced self-consistent models for the Central Dome. The presence of many thin interfingered petrologic units indicates that the intrusions forming the domal core were emplaced over a minimum of 100-220 kyr, and not as a single magma pulse. Isotopic and mineralogical alteration is intense in the upper 100 m but decreases in intensity with depth. Below 800 m, alteration is restricted to narrow zones surrounding faults, veins, igneous contacts, and to an interval of locally intense serpentinization in olivine-rich troctolite. Hydration of the lithosphere occurred over the complete range of temperature conditions from granulite to zeolite facies, but was predominantly in the amphibolite and greenschist range. Deformation of the sequence was remarkably localized, despite paleomagnetic indications that the dome has undergone at least 45 degrees rotation, presumably during unroofing via detachment faulting. Both the deformation pattern and the lithology contrast with what is known from seafloor studies on the adjacent Southern Ridge of the massif. There, the detachment capping the domal core deformed a 100 m thick zone and serpentinized peridotite comprises similar to 70{\%} of recovered samples. We develop a working model of the evolution of Atlantis Massif over the past 2 Myr, outlining several stages that could explain the observed similarities and differences between the Central Dome and the Southern Ridge.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {2169-9313},
	doi = {10.1029/2010JB007931},
	author = {Blackman, D K and Ildefonse, B and John, B E and Ohara, Y and Miller, D J and Abe, N and Abratis, M and Andal, E S and Andreani, M and Awaji, S and Beard, J S and Brunelli, D and Charney, A B and Christie, D M and Collins, J and Delacour, A G and Delius, H and Drouin, M and Einaudi, F and Escartin, J and Frost, B R and Frueh-Green, G and Fryer, P B and Gee, J S and Godard, M and Grimes, C B and Halfpenny, A and Hansen, H -E and Harris, A C and Tamura, A and Hayman, N W and Hellebrand, E and Hirose, T and Hirth, J G and Ishimaru, S and Johnson, K T M and Karner, G D and Linek, M and MacLeod, C J and Maeda, J and Mason, O U and McCaig, A M and Michibayashi, K and Morris, A and Nakagawa, T and Nozaka, T and Rosner, M and Searle, R C and Suhr, G and Tominaga, M and von der Handt, A and Yamasaki, T and Zhao, X}
}
@article {Wanless2011,
	title = {{Volatile abundances and oxygen isotopes in basaltic to dacitic lavas on mid-ocean ridges: The role of assimilation at spreading centers}},
	journal = {Chemical Geology},
	volume = {287},
	number = {1-2},
	year = {2011},
	pages = {54{\textendash}65},
	abstract = {Most geochemical variability in MOR basalts is consistent with low- to moderate-pressure fractional crystallization of various mantle-derived parental melts. However, our geochemical data from MOR high-silica glasses, including new volatile and oxygen isotope data, suggest that assimilation of altered crustal material plays a significant role in the petrogenesis of dacites and may be important in the formation of basaltic lavas at MOR in general. MOR high-silica andesites and dacites from diverse areas show remarkably similar major element trends, incompatible trace element enrichments, and isotopic signatures suggesting similar processes control their chemistry. In particular, very high Cl and elevated H2O concentrations and relatively light oxygen isotope ratios ({\~{}}~5.8{\textperthousand} vs. expected values of {\~{}}~6.8{\textperthousand}) in fresh dacite glasses can be explained by contamination of magmas from a component of ocean crust altered by hydrothermal fluids. Crystallization of silicate phases and Fe-oxides causes an increase in $δ$18O in residual magma, but assimilation of material initially altered at high temperatures results in lower $δ$18O values. The observed geochemical signatures can be explained by extreme fractional crystallization of a MOR basalt parent combined with partial melting and assimilation (AFC) of amphibole-bearing altered oceanic crust. The MOR dacitic lavas do not appear to be simply the extrusive equivalent of oceanic plagiogranites. The combination of partial melting and assimilation produces a distinct geochemical signature that includes higher incompatible trace element abundances and distinct trace element ratios relative to those observed in plagiogranites.},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0009-2541},
	doi = {10.1016/j.chemgeo.2011.05.017},
	url = {http://dx.doi.org/10.1016/j.chemgeo.2011.05.017},
	author = {Wanless, V D and Perfit, M R and Ridley, W I and Wallace, P J and Grimes, C B and Klein, E M}
}
@mastersthesis {Waters2010,
	title = {{Temporal and petrogenetic constraints on volcanic accretionary processes at 9-10 degrees north East Pacific Rise}},
	volume = {Ph.D.},
	year = {2010},
	pages = {258},
	school = {Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution},
	type = {phd},
	address = {Cambridge, MA and Woods Hole, MA},
	abstract = {Volcanic accretion at the fast-spreading East Pacific Rise (EPR) occurs over a {\~{}}2-4 km wide neo-volcanic zone on either side of the axial summit trough (AST). Eruption ages are critical for understanding the distribution and timing of volcanic and magmatic activity. Uranium series nuclides are susceptible to fractionation by magmatic processes that occur beneath mid-ocean ridges, and the half-lives of 226Ra (1.6 kyrs) and 230Th (75 kyrs) make them ideally suited for determining eruption ages and placing constraints on eruption frequency and temporal changes in magma chemistry. Accordingly, major and trace element, and long-lived radiogenic and 238U-230Th-226Ra isotope compositions were measured in basalts from 9{\textordmasculine}-10{\textordmasculine}N EPR to determine eruption ages and to place temporal constraints on volcanic and magmatic processes. At 9{\textordmasculine}30{\textquoteright}N EPR, 238U-230Th-226Ra compositions indicate that trace elementally and isotopically enriched mid-ocean ridge basalt (MORB) collected off-axis erupted {\textgreater}8 ka and that E-MORB magmatism is interspersed with normal, depleted MORB magmatism. Lava ages are consistent with eruption from the AST and flow down the ridge flanks, which is in contrast to previous studies that suggested E-MORB erupted from off-axis vents. At 9{\textordmasculine}50{\textquoteright}N EPR, discrete eruptive units are distinguished by high precision 238U, 232Th, and 226Ra sample concentrations, but because the resolution of the 230Th-226Ra model age dating technique is {\~{}}{\textpm}1 kyrs, the surprisingly young ages of these lavas prohibit the construction of an explicit, time-constrained lava stratigraphy. Nonetheless, seven different flows identified within 0.8-2.0 km west of the AST imply greater frequency of flows to these distances than previously recognized. Model age dating of ferrobasalts, basaltic andesites, andesites, and dacites sampled from the east limb of the overlapping spreading center at 9{\textordmasculine}03{\textquoteright}N EPR is difficult due to uncertainties in magma residence times. However, (226Ra/230Th) disequilibria indicate recent basaltic volcanism ({\textless}{\textless}8 ka) up to {\~{}}4 km off-axis. The axial graben at the rise crest sources the most recent volcanic activity and is the dominant location for eruption of high-silica magmas. Major element, trace element, 87Sr/86Sr, and (234U/238U) isotope compositions are consistent with the formation of dacite magmas by extensive crystallization, and 238U-230Th-226Ra systematics imply crustal residence times of {\~{}}8 kyrs.},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	doi = {10.1575/1912/3750},
	url = {http://hdl.handle.net/1912/3750},
	author = {Waters, C L}
}
@article {Webster2009,
	title = {{Coral reef evolution on rapidly subsiding margins}},
	journal = {Global and Planetary Change},
	volume = {66},
	number = {1-2},
	year = {2009},
	pages = {128{\textendash}148},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0921-8181},
	doi = {10.1016/j.gloplacha.2008.07.010},
	url = {http://dx.doi.org/10.1016/j.gloplacha.2008.07.010},
	author = {Webster, J M and Braga, J C and Clague, D A and Gallup, C and Hein, J R and Potts, D C and Renema, W and Riding, R and Riker-Coleman, K and Silver, E A and Wallace, L M}
}
@article {Blackman2009,
	title = {{Geophysical signatures of oceanic core complexes}},
	journal = {Geophysical Journal International},
	volume = {178},
	number = {2},
	year = {2009},
	month = {aug},
	pages = {593{\textendash}613},
	publisher = {OXFORD UNIV PRESS},
	address = {OXFORD; GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND},
	abstract = {P{\textgreater}Oceanic core complexes (OCCs) provide access to intrusive and ultramafic sections of young lithosphere and their structure and evolution contain clues about how the balance between magmatism and faulting controls the style of rifting that may dominate in a portion of a spreading centre for Myr timescales. Initial models of the development of OCCs depended strongly on insights available from continental core complexes and from seafloor mapping. While these frameworks have been useful in guiding a broader scope of studies and determining the extent of OCC formation along slow spreading ridges, as we summarize herein, results from the past decade highlight the need to reassess the hypothesis that reduced magma supply is a driver of long-lived detachment faulting. The aim of this paper is to review the available geophysical constraints on OCC structure and to look at what aspects of current models are constrained or required by the data. We consider sonar data (morphology and backscatter), gravity, magnetics, borehole geophysics and seismic reflection. Additional emphasis is placed on seismic velocity results (refraction) since this is where deviations from normal crustal accretion should be most readily quantified. However, as with gravity and magnetic studies at OCCs, ambiguities are inherent in seismic interpretation, including within some processing/analysis steps. We briefly discuss some of these issues for each data type. Progress in understanding the shallow structure of OCCs (within similar to 1 km of the seafloor) is considerable. Firm constraints on deeper structure, particularly characterization of the transition from dominantly mafic rock (and/or altered ultramafic rock) to dominantly fresh mantle peridotite, are not currently in hand. There is limited information on the structure and composition of the conjugate lithosphere accreted to the opposite plate while an OCC forms, commonly on the inside corner of a ridge-offset intersection. These gaps preclude full testing of current models. However, with the data in hand there are systematic patterns in OCC structure, such as the 1-2 Myr duration of this rifting style within a given ridge segment, the height of the domal cores with respect to surrounding seafloor, the correspondence of gravity highs with OCCs, and the persistence of corrugations that mark relative (palaeo) slip along the exposed detachment capping the domal cores. This compilation of geophysical results at OCCs should be useful to investigators new to the topic but we also target advanced researchers in our presentation and synthesis of findings to date.},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0956-540X},
	doi = {10.1111/j.1365-246X.2009.04184.x},
	author = {Blackman, D K and Canales, J P and Harding, A}
}
@article {White2009a,
	title = {{Significance of widespread low effusion rate eruptions over the past two million years for delivery of magma to the overlapping spreading centers at 9 degrees N East Pacific Rise}},
	journal = {Earth and Planetary Science Letters},
	volume = {280},
	number = {1-4},
	year = {2009},
	pages = {175{\textendash}184},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/j.epsl.2009.01.030},
	url = {http://dx.doi.org/10.1016/j.epsl.2009.01.030},
	author = {White, S M and Mason, J L and Macdonald, K C and Perfit, M R and Wanless, V D and Klein, E M}
}
@article {German2008,
	title = {{Hydrothermal exploration with the Autonomous Benthic Explorer}},
	journal = {Deep-Sea Research. Part I: Oceanographic Research Papers},
	volume = {55},
	number = {2},
	year = {2008},
	pages = {203{\textendash}219},
	keywords = {AUV ABE (Autonomous Benthic Explorer), AUV Sentry (Autonomous Underwater Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0967-0637},
	doi = {10.1016/j.dsr.2007.11.004},
	url = {http://dx.doi.org/10.1016/j.dsr.2007.11.004},
	author = {German, C R and Yoerger, D R and Jakuba, M V and Shank, T M and Langmuir, C H and Nakamura, K I}
}
@inbook {Humphris2008,
	title = {{Vehicles for deep-sea exploration}},
	booktitle = {Encyclopedia of ocean sciences},
	volume = {6},
	year = {2008},
	pages = {4647{\textendash}4659},
	publisher = {Academic Press},
	organization = {Academic Press},
	address = {San Diego, CA},
	keywords = {AUV ABE (Autonomous Benthic Explorer), AUV Sentry (Autonomous Underwater Vehicle), HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	isbn = {9780123744739},
	doi = {10.1016/B978-012374473-9.00734-7},
	url = {http://dx.doi.org/10.1016/B978-012374473-9.00734-7},
	author = {Humphris, S E},
	editor = {Steele, J H}
}
@article {Hayman2007,
	title = {{Faults and damage zones in fast-spread crust exposed on the north wall of the Hess Deep Rift: Conduits and seals in seafloor hydrothermal systems}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {8},
	year = {2007},
	pages = {Q10002},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2007GC001623},
	url = {http://dx.doi.org/10.1029/2007GC001623},
	author = {Hayman, N W and Karson, J A}
}
@article {Escartin2007,
	title = {{Interplay between faults and lava flows in construction of the upper oceanic crust: The East Pacific Rise crest 9 degrees 25 {\textquoteright}-9 degrees 58 {\textquoteright} N}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {8},
	year = {2007},
	pages = {Q06005},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2006gc001399},
	url = {http://dx.doi.org/10.1029/2006gc001399},
	author = {Escartin, J and Soule, S A and Fornari, D J and Tivey, M A and Schouten, H and Perfit, M R}
}
@mastersthesis {Williams2007,
	title = {{Oceanic lithosphere magnetization: marine magnetic investigations of crustal accretion and tectonic processes in mid-ocean ridge environments}},
	volume = {Ph.D.},
	year = {2007},
	pages = {254},
	school = {Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution},
	type = {phd},
	address = {Cambridge, MA and Woods Hole, MA},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	doi = {10.1575/1912/2031},
	url = {http://hdl.handle.net/1912/2031},
	author = {Williams, C M}
}
@article {Bergmanis2007,
	title = {{Recent eruptive history and magma reservoir dynamics on the southern East Pacific Rise at 17 degrees 30{\textquoteright} S}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {8},
	year = {2007},
	pages = {Q12O06},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2007GC001742},
	url = {http://dx.doi.org/10.1029/2007GC001742},
	author = {Bergmanis, E C and Sinton, J and Rubin, K H}
}
@article {Martinez2006,
	title = {{Opposing trends in crustal thickness and spreading rate along the back-arc Eastern Lau Spreading Center: Implications for controls on ridge morphology, faulting, and hydrothermal activity}},
	journal = {Earth and Planetary Science Letters},
	volume = {245},
	number = {3-4},
	year = {2006},
	pages = {655{\textendash}672},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/j.epsl.2006.03.049},
	url = {http://dx.doi.org/10.1016/j.epsl.2006.03.049},
	author = {Martinez, F and Taylor, B and Baker, E T and Resing, J A and Walker, S L}
}
@article {Tivey2006,
	title = {{Origin of the Pacific Jurassic quiet zone}},
	journal = {Geology},
	volume = {34},
	number = {9},
	year = {2006},
	pages = {789{\textendash}792},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0091-7613},
	doi = {10.1130/g22894.1},
	url = {http://dx.doi.org/10.1130/g22894.1},
	author = {Tivey, M A and Sager, W W and Lee, S M and Tominaga, M}
}
@article {Fryer2006,
	title = {{Variability in serpentinite mudflow mechanisms and sources: ODP drilling results on Mariana forearc seamounts}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {7},
	year = {2006},
	pages = {Q08014},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle), ROV Medea (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2005GC001201},
	url = {http://dx.doi.org/10.1029/2005GC001201},
	author = {Fryer, P and Gharib, J and Ross, K and Savov, I and Mottl, M J}
}
@article {Soule2005,
	title = {{Channelized lava flows at the East Pacific Rise crest 9 degrees-10 degrees N: The importance of off-axis lava transport in developing the architecture of young oceanic crust}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {6},
	year = {2005},
	pages = {Q08005},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2005gc000912},
	url = {http://dx.doi.org/10.1029/2005gc000912},
	author = {Soule, S A and Fornari, D J and Perfit, M R and Tivey, M A and Ridley, W I and Schouten, H}
}
@article {Stewart2005,
	title = {{Four-dimensional upper crustal construction at fast-spreading mid-ocean ridges: A perspective from an upper crustal cross-section at the Hess Deep Rift}},
	journal = {Journal of Volcanology and Geothermal Research},
	volume = {144},
	number = {1-4},
	year = {2005},
	pages = {287{\textendash}309},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0377-0273},
	doi = {10.1016/j.jvolgeores.2004.11.026},
	url = {http://dx.doi.org/10.1016/j.jvolgeores.2004.11.026},
	author = {Stewart, M A and Karson, J A and Klein, E M}
}
@article {Karson2005,
	title = {{Nested-scale investigation of tectonic windows into super-fast spread crust exposed at the Pito Deep Rift}},
	journal = {InterRidge Newsletter},
	volume = {14},
	year = {2005},
	pages = {5{\textendash}8},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	url = {http://www.interridge.org/files/interridge/IR{\_}news{\_}14.pdf},
	author = {Karson, J A and Francheteau, J and Gee, J S and Gillis, K M and Hayman, N W and Hekinian, R and Hey, R N and Hurst, S D and Klein, E M and Naar, D P and Varga, R J and Party, Pito Deep 2005 Scientific}
}
@inbook {Karson2003,
	title = {{Comparison of geologic and seismic structure of uppermost fast-spread oceanic crust: Insights from a crustal cross section at the Hess Deep Rift}},
	booktitle = {Heterogeneity in the Crust and Upper Mantle: Nature, Scaling, and Seismic Properties},
	year = {2003},
	pages = {99{\textendash}129},
	publisher = {Kluwer Academic/Plenum},
	organization = {Kluwer Academic/Plenum},
	address = {New York, N.Y.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	isbn = {0306474476},
	author = {Karson, J A and Christeson, G L},
	editor = {Goff, J A}
}
@article {Stewart2003,
	title = {{Geochemical relationships between dikes and lavas at the Hess Deep Rift: Implications for magma eruptibility}},
	journal = {Journal of Geophysical Research},
	volume = {108},
	number = {B4},
	year = {2003},
	pages = {Art. no. 2184},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2001JB001622},
	url = {http://dx.doi.org/10.1029/2001JB001622},
	author = {Stewart, M A and Klein, E M and Karson, J A and Brophy, J G}
}
@article {Carbotte2003,
	title = {{Magmatic subsidence of the East Pacific Rise (EPR) 18 degrees14{\textquoteright}S revealed through fault restoration of ridge crest bathymetry}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {4},
	number = {1},
	year = {2003},
	pages = {Article no. 1008},
	keywords = {AUV ABE (Autonomous Benthic Explorer), HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2002GC000337},
	url = {http://dx.doi.org/10.1029/2002GC000337},
	author = {Carbotte, S M and Ryan, W B and Cormier, M -H and Jin, W and Bergmanis, E C and Sinton, J and White, S}
}
@article {Engels2003,
	title = {{A new model for submarine volcanic collapse formation}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {4},
	number = {9},
	year = {2003},
	pages = {Article no. 1077},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {1525-2027},
	doi = {10.1029/2002GC000483},
	url = {http://dx.doi.org/10.1029/2002GC000483},
	author = {Engels, J and Edwards, M H and Fornari, D J and Perfit, M R and Cann, J R}
}
@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 {Stewart2002,
	title = {{Geochemistry of dikes and lavas from the north wall of the Hess Deep Rift: Insights into the four-dimensional character of crustal construction at fast spreading mid-ocean ridges}},
	journal = {Journal of Geophysical Research},
	volume = {107},
	number = {B10},
	year = {2002},
	pages = {Art. no. 2238},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2001JB000545},
	url = {http://dx.doi.org/10.1029/2001JB000545},
	author = {Stewart, M A and Klein, E M and Karson, J A}
}
@article {Blackman2002,
	title = {{Geology of the Atlantis Massif (Mid Atlantic Ridge, 30 degrees N): Implications for the evolution of an ultramafic oceanic core complex}},
	journal = {Marine Geophysical Researches},
	volume = {23},
	number = {5-6},
	year = {2002},
	pages = {443{\textendash}469},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0025-3235},
	doi = {10.1023/B:MARI.0000018232.14085.75},
	url = {http://dx.doi.org/10.1023/B:MARI.0000018232.14085.75},
	author = {Blackman, D K and Karson, J A and Kelley, D S and Cann, J R and Fruh-Green, G L and Gee, J S and Hurst, S D and John, B E and Morgan, J and Nooner, S L and Ross, D K and Schroeder, T J and Williams, E A}
}
@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}
}
@article {White2002b,
	title = {{Volcanic mound fields on the East Pacific Rise, 16 degrees -19 degrees S: Low effusion rate eruptions at overlapping spreading centers for the last 1 Myr}},
	journal = {Journal of Geophysical Research},
	volume = {107},
	number = {B10},
	year = {2002},
	pages = {Article no. 2240},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2001JB000483},
	url = {http://dx.doi.org/10.1029/2001JB000483},
	author = {White, S M and Macdonald, K C and Sinton, J M}
}
@book {Fornari2001,
	title = {{AHA-NEMO2: Shipboard data web site compiled during R/V Melville NEMO Expedition, Leg 2, May, 2000}},
	volume = {2005},
	year = {2001},
	keywords = {ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	url = {http://science.whoi.edu/ahanemo2},
	author = {Fornari, D J and Perfit, M R and Tolstoy, M and Haymon, R and Schreirer, D S and Johnson, P and Kurras, G and White, S and Getsiv, J and Party, Shipboard Scientific and Technical}
}
@article {Ballard2001,
	title = {{Deep Black Sea}},
	journal = {National Geographic Magazine},
	volume = {199},
	number = {5},
	year = {2001},
	pages = {52{\textendash}69},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0027-9358},
	author = {Ballard, R D}
}
@article {Smith2001,
	title = {{Magnetic anomalies at the Puna Ridge, a submarine extension of Kilauea Volcano: Implications for lava deposition}},
	journal = {Journal of Geophysical Research},
	volume = {106},
	number = {B8},
	year = {2001},
	pages = {16,16{\textendash}47,60},
	keywords = {ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/2000JB000014},
	url = {http://dx.doi.org/10.1029/2000JB000014},
	author = {Smith, D K and Tivey, M A and Gregg, P and Kong, L}
}
@inbook {Whitcomb2000,
	title = {{Advances in underwater robot vehicles for deep ocean exploration: Navigation, control, and survey operations}},
	booktitle = {Robotics research: the Ninth International Symposium},
	year = {2000},
	pages = {1{\textendash}9},
	publisher = {Springer},
	organization = {Springer},
	address = {New York},
	keywords = {ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	isbn = {1-85233-292-1},
	author = {Whitcomb, L and Yoerger, D R and Singh, H and Howland, J},
	editor = {Hollerbach, J M}
}
@article {Scheirer2000,
	title = {{High-resolution seafloor mapping using the DSL-120 sonar system: Quantitative assessment of sidescan and phase-bathymetry data from the Lucky Strike segment of the Mid-Atlantic Ridge}},
	journal = {Marine Geophysical Researches},
	volume = {21},
	number = {1-2},
	year = {2000},
	month = {feb},
	pages = {121{\textendash}142},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0025-3235},
	doi = {10.1023/A:1004701429848},
	url = {http://dx.doi.org/10.1023/A:1004701429848},
	author = {Scheirer, D S and Fornari, D J and Humphris, S E and Lerner, S}
}
@article {Karson1999a,
	title = {{Large-scale Argo II digital images of upper crustal structures at Hess Deep}},
	journal = {RIDGE Events},
	volume = {10},
	number = {1},
	year = {1999},
	pages = {29{\textendash}32},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	url = {http://www.ridge2000.org/science/downloads/newsletters/R2KNews0699.pdf},
	author = {Karson, J A and Hurst, S D and Klein, E M and Party, Hess Deep {\textquoteright}99 Scientific}
}
@article {White1998,
	title = {{New observations on the distribution of past and present hydrothermal activity in the TAG area of the mid-Atlantic ridge (26 degrees 08 {\textquoteright} N)}},
	journal = {Marine Geophysical Researches},
	volume = {20},
	number = {1},
	year = {1998},
	pages = {41{\textendash}56},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	issn = {0025-3235},
	doi = {10.1023/A:1004376229719},
	url = {http://dx.doi.org/10.1023/A:1004376229719},
	author = {White, S N and Humphris, S E and Kleinrock, M C}
}
@article {Bachmayer1998,
	title = {{Oceanographic research using remotely operated underwater robotic vehicles: exploration of hydrothermal vent sites on the Mid-Atlantic Ridge at 37 North 32 West}},
	journal = {Marine Technology Society Journal},
	volume = {32},
	number = {3},
	year = {1998},
	pages = {37{\textendash}47},
	keywords = {ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle), ROV Medea (Remotely Operated Vehicle)},
	issn = {0025-3324},
	author = {Bachmayer, R and Humphris, S E and Fornari, D J and Van Dover, C L and Howland, J and Bowen, A and Elder, R and Crook, T and Gleason, D E and Sellers, W and Lerner, S}
}
@article {Goff1997,
	title = {{Multiscale spectral analysis of bathymetry on the flank of the Mid-Atlantic Ridge: Modification of the seafloor by mass wasting and sedimentation}},
	journal = {Journal of Geophysical Research},
	volume = {102},
	number = {B7},
	year = {1997},
	pages = {15,415{\textendash}447,462},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0148-0227},
	doi = {10.1029/97JB00723},
	url = {http://dx.doi.org/10.1029/97JB00723},
	author = {Goff, J A and Tucholke, B E}
}
@inbook {Kleinrock1996,
	title = {{Detailed structure and morphology of the TAG active hydrothermal mound and its geotectonic environment}},
	booktitle = {Proceedings of the Ocean Drilling Program, Initial reports},
	volume = {158},
	year = {1996},
	pages = {15{\textendash}21},
	publisher = {Ocean Drilling Program, Texas A{\&}M University},
	organization = {Ocean Drilling Program, Texas A{\&}M University},
	address = {College Station, Tex.},
	keywords = {ROV Argo (Remotely Operated Vehicle), ROV DSL-120 (Remotely Operated Vehicle)},
	doi = {10.2973/odp.proc.ir.158.102.1996},
	url = {http://dx.doi.org/10.2973/odp.proc.ir.158.102.1996},
	author = {Kleinrock, M C and Humphris, S E and Shaw, P and Bowen, A and Crook, T and Davis, C S and Elder, R and Gleason, D E and Goff, J and Goldstein, L and Handley, W and Howland, J and Hussenoeder, S and Koga, K and Lerner, S and Nakamura, K and Rashid, M and Reiser Wetzel, L and Sellers, W and Sulanowska, M and Van Dover, C L and Whitcomb, L},
	editor = {Maddox, E}
}
@mastersthesis {Leader1994,
	title = {{Kalman filter estimation of underwater vehicle position and attitude using Doppler velocity aided inertial motion unit}},
	volume = {O.E.},
	year = {1994},
	pages = {106},
	school = {Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution},
	type = {phd},
	address = {Cambridge, MA and Woods Hole, MA},
	keywords = {ROV DSL-120 (Remotely Operated Vehicle)},
	doi = {10.1575/1912/2418},
	url = {http://hdl.handle.net/1912/2418},
	author = {Leader, D E}
}
