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Volcanic-tectonic structure of the Mt. Dent Oceanic Core Complex in the ultraslow Mid-Cayman Spreading Center determined from detailed seafloor investigation (2019)
Journal Article
Haughton, G., Hayman, N., Searle, R., Le Bas, T., & Murton, B. (2019). Volcanic-tectonic structure of the Mt. Dent Oceanic Core Complex in the ultraslow Mid-Cayman Spreading Center determined from detailed seafloor investigation. Geochemistry, Geophysics, Geosystems, 20(2), 1298-1318. https://doi.org/10.1029/2018gc008032

The flanks of the ultraslow‐spreading Mid‐Cayman Spreading Center (MCSC) are characterized by domal massifs, or oceanic core complexes (OCCs). The most prominent of these, Mt. Dent, comprises lower‐crustal and upper‐mantle lithologies and hosts the V... Read More about Volcanic-tectonic structure of the Mt. Dent Oceanic Core Complex in the ultraslow Mid-Cayman Spreading Center determined from detailed seafloor investigation.

Mid-Ocean Ridges (2013)
Book
Searle, R. (2013). Mid-Ocean Ridges. Cambridge University Press

High-resolution Remotely Operated Vehicle (ROV) mapping of a slow-spreading ridge: Mid-Atlantic Ridge 45°N (2013)
Journal Article
Yeo, I., & Searle, R. (2013). High-resolution Remotely Operated Vehicle (ROV) mapping of a slow-spreading ridge: Mid-Atlantic Ridge 45°N. Geochemistry, Geophysics, Geosystems, 14(6), 1693-1702. https://doi.org/10.1002/ggge.20082

[1] Axial volcanic ridges (AVRs) are found on most slow-spreading mid-ocean ridges and are thought to be the main locus of volcanism there. In this study we present high-resolution mapping of a typical, well-defined AVR on the Mid-Atlantic Ridge at 4... Read More about High-resolution Remotely Operated Vehicle (ROV) mapping of a slow-spreading ridge: Mid-Atlantic Ridge 45°N.

A geophysical study of oceanic core complexes and surrounding terrain, Mid-Atlantic Ridge 13°-14°N (2012)
Journal Article
Mallows, C., & Searle, R. (2012). A geophysical study of oceanic core complexes and surrounding terrain, Mid-Atlantic Ridge 13°-14°N. Geochemistry, Geophysics, Geosystems, 13(6), https://doi.org/10.1029/2012GC004075

We describe a geophysical study of oceanic core complexes (OCC) and surrounding seafloor on the Mid-Atlantic Ridge at 13°N–14°N and off-axis to ∼1.9 Myr. Data include a detailed, deep-towed side scan sonar, magnetic field and bathymetry survey, suppl... Read More about A geophysical study of oceanic core complexes and surrounding terrain, Mid-Atlantic Ridge 13°-14°N.

Eruptive hummocks : building blocks of the upper ocean crust (2012)
Journal Article
Yeo, I., Searle, R. C., Achenbach, K. L., Le Bas, T. P., & Murton, B. J. (2012). Eruptive hummocks : building blocks of the upper ocean crust. Geology, 40(1), 91-94. https://doi.org/10.1130/g31892.1

The spreading axis at many slow-spreading mid-ocean ridges is marked by an axial volcanic ridge. In this study, we use a combination of high-resolution remote sensing methods to elucidate the detailed nature of volcanoes in such a ridge. We find that... Read More about Eruptive hummocks : building blocks of the upper ocean crust.

Hydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre (2012)
Journal Article
Connelly, D., Copley, J., Murton, B., Stansfield, K., Tyler, P., German, C., …Wilcox, S. (2012). Hydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre. Nature Communications, 3, Article 620. https://doi.org/10.1038/ncomms1636

The Mid-Cayman spreading centre is an ultraslow-spreading ridge in the Caribbean Sea. Its extreme depth and geographic isolation from other mid-ocean ridges offer insights into the effects of pressure on hydrothermal venting, and the biogeography of... Read More about Hydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre.

Structure and development of an Axial Volcanic Ridge: Mid-Atlantic Ridge, 45°N (2010)
Journal Article
Searle, R., Murton, B., Achenbach, K., LeBas, T., Tivey, M., Yeo, I., …Waters, C. (2010). Structure and development of an Axial Volcanic Ridge: Mid-Atlantic Ridge, 45°N. Earth and Planetary Science Letters, 299(1-2), 228-241. https://doi.org/10.1016/j.epsl.2010.09.003

We describe the most comprehensive and detailed high resolution survey of an axial volcanic ridge (AVR) ever conducted, at 45°N on the Mid-Atlantic Ridge. We use 3 m resolution sidescan sonar, deep-towed magnetic field measurements, video observation... Read More about Structure and development of an Axial Volcanic Ridge: Mid-Atlantic Ridge, 45°N.

Oceanic core complexes and crustal accretion at slow-spreading ridges (2007)
Journal Article
Ildefonse, B., Blackman, D., John, B., Ohara, Y., Miller, D., MacLeod, C., …Zhao, X. (2007). Oceanic core complexes and crustal accretion at slow-spreading ridges. Geology, 35(7), 623-626. https://doi.org/10.1130/g23531a.1

Oceanic core complexes expose gabbroic rocks on the seafloor via detachment faulting, often associated with serpentinized peridotite. The thickness of these serpentinite units is unknown. Assuming that the steep slopes that typically surround these c... Read More about Oceanic core complexes and crustal accretion at slow-spreading ridges.

Asymmetric generation of oceanic crust at the ultra-slow spreading Southwest Indian Ridge, 64ºE (2007)
Journal Article
Searle, R., & Bralee, A. (2007). Asymmetric generation of oceanic crust at the ultra-slow spreading Southwest Indian Ridge, 64ºE. Geochemistry, Geophysics, Geosystems, 8(1), https://doi.org/10.1029/2006gc001529

We describe topographic, gravity, magnetic, and sonar data from a Southwest Indian Ridge spreading segment near 64E, 28S. We interpret these to reveal crustal structure, spreading history, and volcanic and tectonic processes over the last 12 Myr. We... Read More about Asymmetric generation of oceanic crust at the ultra-slow spreading Southwest Indian Ridge, 64ºE.

Oceanic Core Complex Formation, Atlantis Massif: Expeditions 304 and 305 of the riserless drilling platform from and to Ponta Delgada, Azores (Portugal), Sites U1309–U1311. (2006)
Journal Article
Blackman, D., Ildefonse, B., John, B., Ohara, Y., Miller, D., MacLeod, C., & Scientists, E. 3. (2006). Oceanic Core Complex Formation, Atlantis Massif: Expeditions 304 and 305 of the riserless drilling platform from and to Ponta Delgada, Azores (Portugal), Sites U1309–U1311. Proceedings of the Integrated Ocean Drilling Program, 304/305,