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doi:10.2204/iodp.sp.340T.2011 ReferencesBeard, J.S., Frost, B.R., Fryer, P., McCaig, A., Searle, R., Ildefonse, B., Zinin, P., and Sharma, S.K., 2009. Onset and progression of serpentinization and magnetite formation in olivine-rich troctolite from IODP Hole U1309D. J. Petrol., 50(3):387–403. doi:10.1093/petrology/egp004 Blackman, D.K., Canales, J.P., and Harding, A., 2009. Geophysical signatures of oceanic core complexes. Geophys. J. Int., 178(2):593–613. doi:10.1111/j.1365-246X.2009.04184.x Blackman, D.K., Ildefonse, B., John, B.E., MacLeod, C.J., Ohara, Y., Miller, D.J., and the Expedition 304/305 Project Team, 2004. Oceanic core complex formation, Atlantis Massif—oceanic core complex formation, Atlantis Massif, Mid-Atlantic Ridge: drilling into the footwall and hanging wall of a tectonic exposure of deep, young oceanic lithosphere to study deformation, alteration, and melt generation. IODP Sci. 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Geochem., Geophys., Geosyst., 11(6):Q06003–Q06023. doi:10.1029/2009GC002995 Früh-Green, G.L., Kelley, D.S., Bernasconi, S.M., Karson, J.A., Ludwig, K.A., Butterfield, D.A., Boschi, C., and Proskurowksi, G., 2003. 30,000 years of hydrothermal activity at the Lost City vent field. Science, 301(5632):495–498. doi:10.1126/science.1085582 Godard, M., Abratis, M., Awaji, S., Brunelli, D., Christie, D., Hansen, H., Hellebrand, E., Johnson, K., Maeda, J., Yamasaki, T., and Kato, Y., 2007. Geochemistry of a long in-situ section of intrusive slow-spread crust: results from IODP Site U1309 (Atlantis Massif, 30°N Mid-Atlantic-Ridge). Eos, Trans. Am. Geophys. Union, 88(52)(Suppl.):T53B-1297. (Abstract) http://www.agu.org/meetings/fm07/waisfm07.html Grimes, C.B., John, B.E., Cheadle, M.J., and Wooden, J.L., 2008. Protracted construction of gabbroic crust at a slow spreading ridge: constraints from 206Pb/238U zircon ages from Atlantis Massif and IODP Hole U1309D (30°N, MAR). Geochem., Geophys., Geosyst., 9:Q08012–Q08035. doi:10.1029/2008GC002063 Henig, A.S., Blackman, D.K., Harding, A.J., Kent, G.M., and Canales, J.-P., 2009. Seismic velocity variation within the footwall of an oceanic core complex—Atlantis Massif, Mid-Atlantic Ridge 30°N. InterRidge News, 18:9–13. http://www.interridge.org/files/interridge/IR_News_2009_lowres.pdf Henig, A.S., Blackman, D.K., Harding, A.J., and Kent, G., 2010. Seismic structure and inferred lithology of the heterogeneous upper lithosphere at Atlantis Massif Oceanic Core Complex, 30°N MAR. Eos, Trans. Am. Geophys. Union, 91(Fall Suppl.):T23A-2225. (Abstract) http://www.agu.org/meetings/fm10/waisfm10.html Hirose, T., and Hayman, N.W., 2008. Structure, permeability, and strength of a fault zone in the footwall of an oceanic core complex, the central dome of the Atlantis Massif, Mid-Atlantic Ridge, 30°N. J. Struct. 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