Marguerite Godard1, Julien Collot2, Juerg Matter3, Rupert Sutherland4, Christian Betzler5, Vasileios Chatzaras6, Gaël Erauso7, François Fournier7, Frieder Klein8, Othmar Müntener9, Martin Patriat10, Roy Price11, Shino Suzuki12, *Yasuhiro Yamada13
(1.Université de Montpellier, CNRS, France, 2.Geological Survey of New Caledonia, France, 3.University of Southampton, UK, 4.Victoria University of Wellington, NZ, 5.University Hamburg, Germany, 6.The University of Sydney, Australia, 7.Aix-Marseille Université, France, 8.Woods Hole Oceanographic Insitution, USA, 9.University of Lausanne, Switzerland, 10.Ifremer, France, 11.Stony Brook University, USA, 12.Japan Aerospace Exploration Agency, Japan, 13.Japan Agency for Marine-Earth Science and Technology)
The New Caledonia Ophiolite and its offshore extension to the south (ca. 900km) is one of the world’s largest peridotite massifs, which formed during Eocene subduction initiation. It is an ideal place to study heat and mass exchanges between the solid Earth and its external envelopes, the formation mechanisms of metal and energy resources, the deep biosphere of ultramafic rocks, and impacts on the biological and climate system of both subduction initiation and resultant geochemical fluxes with ultramafic rocks.
We have submitted a preproposal of the New Caledonia Ophiolite Land-to-Sea Drilling Project (NCDP), with proposed drill sites on-land (9 ICDP sites) and off-shore (7 IODP sites). This presentation outlines the proposed scientific objectives and drilling strategy.